2024Article de journal ER2 Auteurs : Chedrewih, Migueli; Medala, Marta; Schmid, Christelle; Garcia, Emmanuel; Damidot, Denis; Thiéry, Vincent Application of various microscopy techniques to study early-age and longer-term behaviour of super sulphated cement microstructure Dans: Journal of Microscopy, vol. 294, no. 2, p. 155-167, 2024, (ACL). Liens @article{chedrewih:hal-04633841,
title = {Application of various microscopy techniques to study early-age and longer-term behaviour of super sulphated cement microstructure},
author = {Migueli Chedrewih and Marta Medala and Christelle Schmid and Emmanuel Garcia and Denis Damidot and Vincent Thiéry},
url = {https://hal.science/hal-04633841},
doi = {10.1111/jmi.13281},
year = {2024},
date = {2024-03-01},
urldate = {2024-03-01},
journal = {Journal of Microscopy},
volume = {294},
number = {2},
pages = {155-167},
publisher = {Wiley},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2024Article de journal ER2 Auteurs : Thiéry, Vincent Barthélémy Faujas de Saint-Fond (1741–1819) and his work on pozzolans and lime: A pioneer in sustainable building Dans: Proceedings of the Geologists' Association, 2024, (ACL). Liens @article{thiery:hal-04560190,
title = {Barthélémy Faujas de Saint-Fond (1741–1819) and his work on pozzolans and lime: A pioneer in sustainable building},
author = {Vincent Thiéry},
url = {https://imt-nord-europe.hal.science/hal-04560190},
doi = {10.1016/j.pgeola.2024.04.004},
year = {2024},
date = {2024-04-01},
urldate = {2024-04-01},
journal = {Proceedings of the Geologists' Association},
publisher = {Elsevier},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2023Article de journal ER2 Auteurs : Chedrewih, Migueli; Thiéry, Vincent; Gauthier, Arnaud; Amin, Fouad Incorporation of antimony-bearing mining wastes into clinker Portland raw feed: The difficulty of Sb analysis in calcium silicates Dans: Journal of Microscopy, 2023, (ACL). Liens @article{chedrewih:hal-04237014,
title = {Incorporation of antimony-bearing mining wastes into clinker Portland raw feed: The difficulty of Sb analysis in calcium silicates},
author = {Migueli Chedrewih and Vincent Thiéry and Arnaud Gauthier and Fouad Amin},
url = {https://imt-nord-europe.hal.science/hal-04237014},
doi = {10.1111/jmi.13228},
year = {2023},
date = {2023-09-01},
urldate = {2023-09-01},
journal = {Journal of Microscopy},
publisher = {Wiley},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2022Article de journal ER2 Auteurs : Thiéry, Vincent; Dubois, Emmanuel; Bellayer, Séverine The good, the bad and the ugly polishing: Effect of abrasive size on standardless EDS analysis of Portland cement clinker's calcium silicates Dans: Micron, vol. 158, p. 103266, 2022, (ACL). Liens @article{thiery:hal-03662917,
title = {The good, the bad and the ugly polishing: Effect of abrasive size on standardless EDS analysis of Portland cement clinker's calcium silicates},
author = {Vincent Thiéry and Emmanuel Dubois and Séverine Bellayer},
url = {https://hal.archives-ouvertes.fr/hal-03662917},
doi = {10.1016/j.micron.2022.103266},
year = {2022},
date = {2022-07-01},
urldate = {2022-07-01},
journal = {Micron},
volume = {158},
pages = {103266},
publisher = {Elsevier},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2021Article de journal ER2 Auteurs : Colman, C; Bulteel, David; Thiery, Vincent; é, S R; Michel, F; Courard, L Internal sulfate attack in mortars containing contaminated fine recycled concrete aggregates Dans: Construction and Building Materials, vol. 272, p. 121851, 2021, (ACL). Liens @article{Colman2021,
title = {Internal sulfate attack in mortars containing contaminated fine recycled concrete aggregates},
author = {C Colman and David Bulteel and Vincent Thiery and S R é and F Michel and L Courard},
doi = {10.1016/j.conbuildmat.2020.121851},
year = {2021},
date = {2021-02-01},
journal = {Construction and Building Materials},
volume = {272},
pages = {121851},
publisher = {Elsevier BV},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2021Article de journal ER2 Auteurs : Thiéry, Vincent Metamorphism of sedimentary rocks recognised by 19th century French naturalists: A case study from the Chavanon sequence marbles, Massif Central, France Dans: Proceedings of the Geologists' Association, vol. 132, no. 4, p. 491-496, 2021, ISSN: 0016-7878, (ACL). Résumé | Liens @article{THIERY2021491,
title = {Metamorphism of sedimentary rocks recognised by 19th century French naturalists: A case study from the Chavanon sequence marbles, Massif Central, France},
author = {Vincent Thiéry},
url = {https://www.sciencedirect.com/science/article/pii/S0016787821000432},
doi = {https://doi.org/10.1016/j.pgeola.2021.05.003},
issn = {0016-7878},
year = {2021},
date = {2021-01-01},
urldate = {2021-01-01},
journal = {Proceedings of the Geologists' Association},
volume = {132},
number = {4},
pages = {491-496},
abstract = {The Chavanon metamorphic sequence in the Variscan French Massif Central contains marble lenses that have been exploited since at least the 18th century to produce lime. They provided an opportunity to some major pioneers among nineteenth century French geologists to understand how metamorphic rocks are formed. The intimate association between marbles and gneisses led them to propose that the initial pile of rocks was deposited as a single unit under water. They thoroughly described the attitude, folding and mineralogy of the marbles, making their works of great historical value. Originally written in French, their translation into English and the reproduction of original figures from the works they published will be very useful to the international community of geologists interested in the history of their science.},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
The Chavanon metamorphic sequence in the Variscan French Massif Central contains marble lenses that have been exploited since at least the 18th century to produce lime. They provided an opportunity to some major pioneers among nineteenth century French geologists to understand how metamorphic rocks are formed. The intimate association between marbles and gneisses led them to propose that the initial pile of rocks was deposited as a single unit under water. They thoroughly described the attitude, folding and mineralogy of the marbles, making their works of great historical value. Originally written in French, their translation into English and the reproduction of original figures from the works they published will be very useful to the international community of geologists interested in the history of their science. |
2019Article de journal ER2 Auteurs : Thiéry, Vincent Le pont Charles-Marlin (Saint-Georges-Nigremont, Creuse). Historique et caractérisation préliminaire des désordres Dans: Annales du Bâtiment et des Travaux Publics, vol. 70, no. 5-6, p. 7–18, 2019, (ACL). @article{Thiery2019,
title = {Le pont Charles-Marlin (Saint-Georges-Nigremont, Creuse). Historique et caractérisation préliminaire des désordres},
author = {Vincent Thiéry},
year = {2019},
date = {2019-01-01},
journal = {Annales du Bâtiment et des Travaux Publics},
volume = {70},
number = {5-6},
pages = {7--18},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2019Article de journal ER2 Auteurs : Thiéry, Vincent À la recherche des ciments oubliés Dans: Mines & Carrières, vol. 275, p. 22–25, 2019, (OV). @article{Thiery2019a,
title = {À la recherche des ciments oubliés},
author = {Vincent Thiéry},
year = {2019},
date = {2019-01-01},
journal = {Mines & Carrières},
volume = {275},
pages = {22--25},
note = {OV},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2019Proceedings Article ER2 Auteurs : Thiéry, Vincent Microstructural investigations on an abandoned 1935 concrete bridge Dans: 16th Euroseminars on Microscopy Applied to Building Materials (EMABM), p. 289–294, 2019, (ACTI). @inproceedings{Thiery2019b,
title = {Microstructural investigations on an abandoned 1935 concrete bridge},
author = {Vincent Thiéry},
year = {2019},
date = {2019-01-01},
booktitle = {16th Euroseminars on Microscopy Applied to Building Materials (EMABM)},
pages = {289--294},
note = {ACTI},
keywords = {ER2},
pubstate = {published},
tppubtype = {inproceedings}
}
|
2019Article de journal ER2 Auteurs : Urupina, D; Lasne, J; Romanias, M N; Thiéry, Vincent; Dagsson-Waldhauserova, P; Thevenet, F Uptake and surface chemistry of SO2 on natural volcanic dusts Dans: Atmospheric Environment, vol. 217, p. 116942, 2019, ISSN: 1352-2310, (ACL). Résumé | Liens @article{URUPINA2019116942,
title = {Uptake and surface chemistry of SO2 on natural volcanic dusts},
author = {D Urupina and J Lasne and M N Romanias and Vincent Thiéry and P Dagsson-Waldhauserova and F Thevenet},
url = {http://www.sciencedirect.com/science/article/pii/S1352231019305813},
doi = {https://doi.org/10.1016/j.atmosenv.2019.116942},
issn = {1352-2310},
year = {2019},
date = {2019-01-01},
journal = {Atmospheric Environment},
volume = {217},
pages = {116942},
abstract = {V-dust (v-dust) is a highly variable source of natural particles in the atmosphere, and during the period of high volcanic activity it can provide a large surface for heterogeneous interactions with other atmospheric compounds. Icelandic v-dust was chosen as a case study due to frequency of volcanic eruptions and high aeolian activity in the area. In this study, we focus on the kinetics and mechanism of the reaction of sulfur dioxide (SO2) with natural v-dust samples under atmospheric conditions using coated wall flow tube reactor and diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). Steady state uptake coefficients determined are in the range of 10−9 to 10−8 depending on the considered v-dust. Concomitantly with SO2 uptake, both sulfites and sulfates are monitored on the surface of v-dust, with sulfates being the final oxidation product, attesting of SO2 surface reaction. Surface hydroxyl groups play a crucial role in the conversion of SO2 to sulfites as evidenced from both flow tube and DRIFTS experiments. Based on these experimental results, a mechanism for SO2 interaction with different surface sites of v-dust is proposed and discussed. This study provides original insights in the kinetics of SO2 uptake under simulated atmospheric conditions and its mechanism and transformation on volcanic material. To that regards, it brings an accurate perspective on SO2 heterogeneous sinks in the atmosphere.},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
V-dust (v-dust) is a highly variable source of natural particles in the atmosphere, and during the period of high volcanic activity it can provide a large surface for heterogeneous interactions with other atmospheric compounds. Icelandic v-dust was chosen as a case study due to frequency of volcanic eruptions and high aeolian activity in the area. In this study, we focus on the kinetics and mechanism of the reaction of sulfur dioxide (SO2) with natural v-dust samples under atmospheric conditions using coated wall flow tube reactor and diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). Steady state uptake coefficients determined are in the range of 10−9 to 10−8 depending on the considered v-dust. Concomitantly with SO2 uptake, both sulfites and sulfates are monitored on the surface of v-dust, with sulfates being the final oxidation product, attesting of SO2 surface reaction. Surface hydroxyl groups play a crucial role in the conversion of SO2 to sulfites as evidenced from both flow tube and DRIFTS experiments. Based on these experimental results, a mechanism for SO2 interaction with different surface sites of v-dust is proposed and discussed. This study provides original insights in the kinetics of SO2 uptake under simulated atmospheric conditions and its mechanism and transformation on volcanic material. To that regards, it brings an accurate perspective on SO2 heterogeneous sinks in the atmosphere. |
2019Article de journal ER2 Auteurs : Thiéry, Vincent Le mouvement de versant d'Arpiat dans la vallée de la Dordogne Dans: Revue des sciences naturelles d'Auvergne, vol. 83, p. 49–56, 2019, (ACL). @article{Thiery2019c,
title = {Le mouvement de versant d'Arpiat dans la vallée de la Dordogne},
author = {Vincent Thiéry},
year = {2019},
date = {2019-01-01},
journal = {Revue des sciences naturelles d'Auvergne},
volume = {83},
pages = {49--56},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2018Article de journal ER2 Auteurs : Bourdot, A; Thiéry, Vincent; Bulteel, David; Cuchet, S; Hammerschlag, J -G Alkali-reactivity of a Swiss siliceous limestone caused by finely dispersed quartz Dans: Cement and Concrete Composites, vol. 91, 2018, ISSN: 09589465. Résumé | Liens @article{Bourdot2018,
title = {Alkali-reactivity of a Swiss siliceous limestone caused by finely dispersed quartz},
author = {A Bourdot and Vincent Thiéry and David Bulteel and S Cuchet and J -G Hammerschlag},
doi = {10.1016/j.cemconcomp.2018.04.016},
issn = {09589465},
year = {2018},
date = {2018-01-01},
journal = {Cement and Concrete Composites},
volume = {91},
abstract = {textcopyright 2018 Elsevier Ltd The present study was conducted to provide a better understanding of the alkali-silica reactivity (ASR) of siliceous limestones in concrete applications. A Swiss siliceous limestone, which is potentially reactive, was subjected to a series of tests. Microbar tests were first conducted to classify the limestones reactivity with respect to ASR. Two other methods were then used to characterize the amount of SiO 2 present. First, an analysis of the chemical composition with petrographic and mineralogical characterizations was carried out, and second, a model reactor was used to characterize the silica reactivity. The results showed a siliceous reactive limestone. In petrography, three main types of carbonate lithology were outlined according to their SiO 2 and glauconitic content. The emphasis was placed on the types of SiO 2 and their sizes: a finely dispersed micro- to crypto-quartz has been highlighted by SEM and TEM, and analysed as quartz. The reactive free SiO 2 content, obtained by a mineralogical calculating method, completes the petrographic results. The proportion of reactive free SiO 2 could be essentially attributed to the presence of finely dispersed micro- to crypto-quartz from TEM observations which is probably very reactive towards the ASR due to its small-size. The presence of finely dispersed micro- to crypto-quartz is important to consider, due to its potential effects on the concrete mixture. The grain size of SiO 2 seems to be a supplementary key parameter, in addition to crystallinity and strain, since it can promote ASR development with some siliceous aggregates.},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
textcopyright 2018 Elsevier Ltd The present study was conducted to provide a better understanding of the alkali-silica reactivity (ASR) of siliceous limestones in concrete applications. A Swiss siliceous limestone, which is potentially reactive, was subjected to a series of tests. Microbar tests were first conducted to classify the limestones reactivity with respect to ASR. Two other methods were then used to characterize the amount of SiO 2 present. First, an analysis of the chemical composition with petrographic and mineralogical characterizations was carried out, and second, a model reactor was used to characterize the silica reactivity. The results showed a siliceous reactive limestone. In petrography, three main types of carbonate lithology were outlined according to their SiO 2 and glauconitic content. The emphasis was placed on the types of SiO 2 and their sizes: a finely dispersed micro- to crypto-quartz has been highlighted by SEM and TEM, and analysed as quartz. The reactive free SiO 2 content, obtained by a mineralogical calculating method, completes the petrographic results. The proportion of reactive free SiO 2 could be essentially attributed to the presence of finely dispersed micro- to crypto-quartz from TEM observations which is probably very reactive towards the ASR due to its small-size. The presence of finely dispersed micro- to crypto-quartz is important to consider, due to its potential effects on the concrete mixture. The grain size of SiO 2 seems to be a supplementary key parameter, in addition to crystallinity and strain, since it can promote ASR development with some siliceous aggregates. |
2018Article de journal ER2 Auteurs : Maimouni, H; Remond, S; Huchet, F; Richard, P; Thiéry, Vincent; Descantes, Y Quantitative assessment of the saturation degree of model fine recycled concrete aggregates immersed in a filler or cement paste Dans: Construction and Building Materials, vol. 175, 2018, ISSN: 09500618. Résumé | Liens @article{Maimouni2018,
title = {Quantitative assessment of the saturation degree of model fine recycled concrete aggregates immersed in a filler or cement paste},
author = {H Maimouni and S Remond and F Huchet and P Richard and Vincent Thiéry and Y Descantes},
doi = {10.1016/j.conbuildmat.2018.04.211},
issn = {09500618},
year = {2018},
date = {2018-01-01},
journal = {Construction and Building Materials},
volume = {175},
abstract = {textcopyright 2018 We study water transfer between different model fine recycled concrete aggregates and fresh filler or cement paste in which they are immersed. Our aim is to introduce a spread based experimental protocol for studying the time evolution of water content in initially dry aggregates when mixed with such pastes. The procedure developed hereby is tested on three model Cement Paste Sands (CPS) prepared with different water-to-cement ratios leading to very different porosities and pore structures. The results show that water content in the CPS reaches a maximum no later than 6 min after first contact with limestone filler or cement paste then remains fairly constant afterwards. The saturation degree, i.e. ratio of the water content in the CPS to their water absorption, increases with the porosity of the CPS and remains less than one whatever the paste. The corresponding reduction of water absorption capacity in a cement paste should be taken into account during mix design of a recycled concrete.},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
textcopyright 2018 We study water transfer between different model fine recycled concrete aggregates and fresh filler or cement paste in which they are immersed. Our aim is to introduce a spread based experimental protocol for studying the time evolution of water content in initially dry aggregates when mixed with such pastes. The procedure developed hereby is tested on three model Cement Paste Sands (CPS) prepared with different water-to-cement ratios leading to very different porosities and pore structures. The results show that water content in the CPS reaches a maximum no later than 6 min after first contact with limestone filler or cement paste then remains fairly constant afterwards. The saturation degree, i.e. ratio of the water content in the CPS to their water absorption, increases with the porosity of the CPS and remains less than one whatever the paste. The corresponding reduction of water absorption capacity in a cement paste should be taken into account during mix design of a recycled concrete. |
2018Article de journal ER2 Auteurs : Trincal, V; Thiéry, Vincent; Mamindy-Pajany, Yannick; Hillier, S Use of hydraulic binders for reducing sulphate leaching: application to gypsiferous soil sampled in Ile-de-France region (France) Dans: Environmental Science and Pollution Research, 2018, ISSN: 16147499. Résumé | Liens @article{Trincal2018,
title = {Use of hydraulic binders for reducing sulphate leaching: application to gypsiferous soil sampled in Ile-de-France region (France)},
author = {V Trincal and Vincent Thiéry and Yannick Mamindy-Pajany and S Hillier},
doi = {10.1007/s11356-018-2376-5},
issn = {16147499},
year = {2018},
date = {2018-01-01},
journal = {Environmental Science and Pollution Research},
abstract = {textcopyright 2018 Springer-Verlag GmbH Germany, part of Springer Nature Polluted soils are a serious environmental risk worldwide and consist of millions of tons of mineral waste to be treated. In order to ensure their sustainable management, various remediation options must be considered. Hydraulic binder treatment is one option that may allow a stabilisation of pollution and thus offer a valorisation as secondary raw materials rather than considering them as waste. In this study, we focused on sulphate-polluted soil and tested the effectiveness of several experimental hydraulic binders. The aim was to transform gypsum into ettringite, a much less soluble sulphate, and therefore to restrict the potential for sulphate pollutant release. The environmental assessment of five formulations using hydraulic binders was compared to the gypsiferous soil before treatment (contaminated in sulphate). The approach was to combine leaching tests with mineralogical quantifications using among others thermogravimetric and XRD methods. In the original soil and in the five formulations, leaching tests indicate sulphate release above environmental standards. However, hydraulic binders promote ettringite formation, as well as a gypsum content reduction as observed by SEM. The stabilisation of sulphates is, however, insufficient, probably as a result of the very high content of gypsum in the unusual soil used. The mineralogical reactions highlighted during the hydration of hydraulic binders are promising; they could pave the way for the development of new industrial mixtures that would have a positive environmental impact by allowing reuse of soils that would otherwise be classified as waste.},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
textcopyright 2018 Springer-Verlag GmbH Germany, part of Springer Nature Polluted soils are a serious environmental risk worldwide and consist of millions of tons of mineral waste to be treated. In order to ensure their sustainable management, various remediation options must be considered. Hydraulic binder treatment is one option that may allow a stabilisation of pollution and thus offer a valorisation as secondary raw materials rather than considering them as waste. In this study, we focused on sulphate-polluted soil and tested the effectiveness of several experimental hydraulic binders. The aim was to transform gypsum into ettringite, a much less soluble sulphate, and therefore to restrict the potential for sulphate pollutant release. The environmental assessment of five formulations using hydraulic binders was compared to the gypsiferous soil before treatment (contaminated in sulphate). The approach was to combine leaching tests with mineralogical quantifications using among others thermogravimetric and XRD methods. In the original soil and in the five formulations, leaching tests indicate sulphate release above environmental standards. However, hydraulic binders promote ettringite formation, as well as a gypsum content reduction as observed by SEM. The stabilisation of sulphates is, however, insufficient, probably as a result of the very high content of gypsum in the unusual soil used. The mineralogical reactions highlighted during the hydration of hydraulic binders are promising; they could pave the way for the development of new industrial mixtures that would have a positive environmental impact by allowing reuse of soils that would otherwise be classified as waste. |
2018Chapitre d'ouvrage ER2 Auteurs : Kruszewski, Łukasz; Gatel, Pierre; Thiéry, Vincent; Moszumańska, Izabela; Kusy, Danuta Crystallochemical Behavior of Slag Minerals and the Occurrence of Potentially New Mineral Species From Lapanouse-de-Sévérac, France Dans: Coal and Peat Fires: A Global Perspective, p. 243–300, 2018, (OS). Liens @inbook{inbook,
title = {Crystallochemical Behavior of Slag Minerals and the Occurrence of Potentially New Mineral Species From Lapanouse-de-Sévérac, France},
author = {Łukasz Kruszewski and Pierre Gatel and Vincent Thiéry and Izabela Moszumańska and Danuta Kusy},
doi = {10.1016/B978-0-12-849885-9.00013-5},
year = {2018},
date = {2018-01-01},
booktitle = {Coal and Peat Fires: A Global Perspective},
pages = {243--300},
note = {OS},
keywords = {ER2},
pubstate = {published},
tppubtype = {inbook}
}
|
2018Chapitre d'ouvrage ER2 Auteurs : Thiéry, Vincent; Guy, B; Kruszewski, Ł; Carpentier, J F The burning coal heap at La Ricamarie, Loire Coal Basin, France Dans: Stracher, G B (Ed.): Coal and Peat Fires: A Global Perspective. Volume 5 : case studies - advances in field and laboratory research, p. 301–331, 2018, (OS). @inbook{Thiery2018,
title = {The burning coal heap at La Ricamarie, Loire Coal Basin, France},
author = {Vincent Thiéry and B Guy and Ł Kruszewski and J F Carpentier},
editor = {G B Stracher},
year = {2018},
date = {2018-01-01},
booktitle = {Coal and Peat Fires: A Global Perspective. Volume 5 : case studies - advances in field and laboratory research},
pages = {301--331},
note = {OS},
keywords = {ER2},
pubstate = {published},
tppubtype = {inbook}
}
|
2017Proceedings Article ER2 Auteurs : Thiéry, Vincent; Link, G; Katayama, T; Ando, Y; Bouichou, M; Marie-Victoire, E Preliminary study of 19th century mortars from railway engineering structures abandoned since 1950 Dans: Euroseminars on Microscopy Applied to Building Materials (EMABM), 2017. @inproceedings{Thiery2017a,
title = {Preliminary study of 19th century mortars from railway engineering structures abandoned since 1950},
author = {Vincent Thiéry and G Link and T Katayama and Y Ando and M Bouichou and E Marie-Victoire},
year = {2017},
date = {2017-01-01},
booktitle = {Euroseminars on Microscopy Applied to Building Materials (EMABM)},
keywords = {ER2},
pubstate = {published},
tppubtype = {inproceedings}
}
|
2017Article de journal ER2 Auteurs : Thiéry, Vincent; Trincal, V; Davy, C The elusive ettringite under the high-vacuum SEM - a reflection based on natural samples, the use of Monte-Carlo modeling of EDS analyses, and an extension to the ettringite group minerals Dans: Journal of Microscopy, vol. 268, p. 84–93, 2017. @article{Thiery2017,
title = {The elusive ettringite under the high-vacuum SEM - a reflection based on natural samples, the use of Monte-Carlo modeling of EDS analyses, and an extension to the ettringite group minerals},
author = {Vincent Thiéry and V Trincal and C Davy},
year = {2017},
date = {2017-01-01},
journal = {Journal of Microscopy},
volume = {268},
pages = {84--93},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2016Article de journal ER4 Auteurs : Thiéry, Vincent; Rolin, Patrick; Dubois, Michel; Caumon, Marie-Camille; Goncalves, Philippe Reply to J. Berger's comment on the article “Discovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif” by Thiéry, V. et al.,. (2015), Gondwana Research 28, 954–960 Dans: Gondwana Research, vol. 38, p. 372-374, 2016, (ACL). Résumé @article{Thiery2016,
title = {Reply to J. Berger's comment on the article “Discovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif” by Thiéry, V. et al.,. (2015), Gondwana Research 28, 954–960},
author = {Vincent Thiéry and Patrick Rolin and Michel Dubois and Marie-Camille Caumon and Philippe Goncalves},
year = {2016},
date = {2016-01-01},
journal = {Gondwana Research},
volume = {38},
pages = {372-374},
abstract = {We are pleased to see that our recently published article (thiéry et al., 2015) is discussed (berger, 2015); in the following lines we will give some precisions and thoughts about the comment. this is not the first time that a documentation of microdiamond within metamorphic terranes is discussed (mposkos and kostopoulos, 2001; beyssac and chopin, 2003; mposkos and kostopoulos, 2003), revealing the complexity of the unraveling of uhp metamorphism. several points are to be addressed, concerning both the need for precision about the samples themselves and the need for a more thorough estimation of p–t conditions},
note = {ACL},
keywords = {ER4},
pubstate = {published},
tppubtype = {article}
}
We are pleased to see that our recently published article (thiéry et al., 2015) is discussed (berger, 2015); in the following lines we will give some precisions and thoughts about the comment. this is not the first time that a documentation of microdiamond within metamorphic terranes is discussed (mposkos and kostopoulos, 2001; beyssac and chopin, 2003; mposkos and kostopoulos, 2003), revealing the complexity of the unraveling of uhp metamorphism. several points are to be addressed, concerning both the need for precision about the samples themselves and the need for a more thorough estimation of p–t conditions |
2016Article de journal ER2 Auteurs : Thiéry, Vincent Entre folklore, archéologie et géologie: la Roche Mandrin (Larodde, 63) Dans: Bulletin de la Société d'Histoire Naturelle d'Auvergne, vol. 80, p. 17–26, 2016. @article{Thiery2016b,
title = {Entre folklore, archéologie et géologie: la Roche Mandrin (Larodde, 63)},
author = {Vincent Thiéry},
year = {2016},
date = {2016-01-01},
journal = {Bulletin de la Société d'Histoire Naturelle d'Auvergne},
volume = {80},
pages = {17--26},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2016Proceedings Article ER2 Auteurs : Song, Y; Davy, C; Thiéry, Vincent; Troadec, D; Damidot, D Multi-scale assessment of the 3D pore network of a high performance concrete Dans: Proceedings of the 38th International Conference on Cement Microscopy, 2016, ISBN: 193078712X. @inproceedings{Song2016,
title = {Multi-scale assessment of the 3D pore network of a high performance concrete},
author = {Y Song and C Davy and Vincent Thiéry and D Troadec and D Damidot},
isbn = {193078712X},
year = {2016},
date = {2016-01-01},
booktitle = {Proceedings of the 38th International Conference on Cement Microscopy},
keywords = {ER2},
pubstate = {published},
tppubtype = {inproceedings}
}
|
2016Proceedings Article ER2 Auteurs : Thiéry, Vincent; Meulenyzer, S; Bouichou, M; Marie-Victoire, E Some historical points about cementand microscopy in France Dans: Proceedings of the 38th International Conference on Cement Microscopy, 2016, ISBN: 193078712X. Résumé @inproceedings{Thiery2016a,
title = {Some historical points about cementand microscopy in France},
author = {Vincent Thiéry and S Meulenyzer and M Bouichou and E Marie-Victoire},
isbn = {193078712X},
year = {2016},
date = {2016-01-01},
booktitle = {Proceedings of the 38th International Conference on Cement Microscopy},
abstract = {France and cement microscopy are intimately linked since the pioneering works of the famous chemist Henry Le Chatelier (1850-1936) who was the first to use the petrographic microscope to describe the phases of Portland clinker and the products of cement hydration. Based on a selection of historical documents and samples, we will give a historical and technical overview of cement and binders, in the broadest sense, in France. We will cover several centuries, from the Roman aqueduct 'Pont du Gard' (1st century A.D.) to the first Portland-cement based bridge 'Pont de Souillac' built by Louis Vicat from 1812 to 1824, from the natural cements made in Burgundy to the ultrahigh performance decorative concrete used in modern architecture. In Burgundy, we will see the case of the Vassy church, built in 1859 by Gariel, a Vassy natural cement producer. Then, cement mortars from the 19th century, used for the restoration of the Saint-Pierre-et-Saint-Paul Cathedral portal in Troyes, will be presented.},
keywords = {ER2},
pubstate = {published},
tppubtype = {inproceedings}
}
France and cement microscopy are intimately linked since the pioneering works of the famous chemist Henry Le Chatelier (1850-1936) who was the first to use the petrographic microscope to describe the phases of Portland clinker and the products of cement hydration. Based on a selection of historical documents and samples, we will give a historical and technical overview of cement and binders, in the broadest sense, in France. We will cover several centuries, from the Roman aqueduct 'Pont du Gard' (1st century A.D.) to the first Portland-cement based bridge 'Pont de Souillac' built by Louis Vicat from 1812 to 1824, from the natural cements made in Burgundy to the ultrahigh performance decorative concrete used in modern architecture. In Burgundy, we will see the case of the Vassy church, built in 1859 by Gariel, a Vassy natural cement producer. Then, cement mortars from the 19th century, used for the restoration of the Saint-Pierre-et-Saint-Paul Cathedral portal in Troyes, will be presented. |
2016Article de journal ER2 Auteurs : Bourdot, Alexandra; Thiéry, Vincent; Bulteel, David; Hammerschlag, Jean-Gabriel Effect of burnt oil shale on ASR expansions: A petrographic study of concretes based on reactive aggregates Dans: Construction and Building Materials, vol. 112, p. 556–569, 2016, (ACL). Liens @article{Bourdot2016,
title = {Effect of burnt oil shale on ASR expansions: A petrographic study of concretes based on reactive aggregates},
author = {Alexandra Bourdot and Vincent Thiéry and David Bulteel and Jean-Gabriel Hammerschlag},
doi = {10.1016/j.conbuildmat.2016.02.148},
year = {2016},
date = {2016-06-01},
journal = {Construction and Building Materials},
volume = {112},
pages = {556--569},
publisher = {Elsevier BV},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2015Article de journal ER4 Auteurs : Thiéry, Vincent; Rolin, Patrick; Dubois, Michel; Caumon, Marie-Camille Discovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif Central Dans: Gondwana Research, vol. 28, no. 3, p. 954-960, 2015, (ACL). Résumé @article{Thiery2015,
title = {Discovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif Central},
author = {Vincent Thiéry and Patrick Rolin and Michel Dubois and Marie-Camille Caumon},
year = {2015},
date = {2015-01-01},
journal = {Gondwana Research},
volume = {28},
number = {3},
pages = {954-960},
abstract = {The variscan french massif central (fmc) is classically described as a stack of nappes with increasing metamorphism from the bottom (parautochthonous unit) to the top (lower and upper gneiss units). ultra-high pressure (uhp) metamorphism was already recognized in the uppermost units, with notably coesite-bearing rocks. we report the first finding of metamorphic microdiamonds in the parautochthonous unit, revealing that the uhp event affected the whole stack of nappes and also that the pressures reached are above what was previously expected, since the presence of diamond, according to the peak temperature estimates for this unit, indicates pressures of ca. 3 gpa (i.e. 100 km depth). at the scale of the fmc, this finding adds complexity to the established models. on a broader scale, this adds evidence of similarity between this part of the belt and other uhp variscan terranes such as the erzgebirge and the bohemian massif},
note = {ACL},
keywords = {ER4},
pubstate = {published},
tppubtype = {article}
}
The variscan french massif central (fmc) is classically described as a stack of nappes with increasing metamorphism from the bottom (parautochthonous unit) to the top (lower and upper gneiss units). ultra-high pressure (uhp) metamorphism was already recognized in the uppermost units, with notably coesite-bearing rocks. we report the first finding of metamorphic microdiamonds in the parautochthonous unit, revealing that the uhp event affected the whole stack of nappes and also that the pressures reached are above what was previously expected, since the presence of diamond, according to the peak temperature estimates for this unit, indicates pressures of ca. 3 gpa (i.e. 100 km depth). at the scale of the fmc, this finding adds complexity to the established models. on a broader scale, this adds evidence of similarity between this part of the belt and other uhp variscan terranes such as the erzgebirge and the bohemian massif |
2015Article de journal ER2 Auteurs : Thiery, Vincent; Rolin, Patrick; Dubois, Michel; Caumon, Marie-Camille Điscovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif Central Dans: Gondwana Research, vol. 28, no. 3, p. 954-960, 2015, (ACL). Résumé @article{THIE2015A,
title = {Điscovery of metamorphic microdiamonds from the parautochthonous units of the Variscan French Massif Central},
author = {Vincent Thiery and Patrick Rolin and Michel Dubois and Marie-Camille Caumon},
year = {2015},
date = {2015-01-01},
journal = {Gondwana Research},
volume = {28},
number = {3},
pages = {954-960},
abstract = {The Variscan French Massif Central (FMC) is classically described as a stack of nappes with increasing metamorphism from the bottom (parautochthonous unit) to the top (lower and upper gneiss units). Ultra-high pressure (UHP) metamorphism was already recognized in the uppermost units, with notably coesite-bearing rocks. We report the first finding of metamorphic microdiamonds in the parautochthonous unit, revealing that the UHP event affected the whole stack of nappes and also that the pressures reached are above what was previously expected, since the presence of diamond, according to the peak temperature estimates for this unit, indicates pressures of ca. 3 GPa (i.e. 100 km depth). At the scale of the FMC, this finding adds complexity to the established models. On a broader scale, this adds evidence of similarity between this part of the belt and other UHP Variscan terranes such as the Erzgebirge and the Bohemian Massif},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
The Variscan French Massif Central (FMC) is classically described as a stack of nappes with increasing metamorphism from the bottom (parautochthonous unit) to the top (lower and upper gneiss units). Ultra-high pressure (UHP) metamorphism was already recognized in the uppermost units, with notably coesite-bearing rocks. We report the first finding of metamorphic microdiamonds in the parautochthonous unit, revealing that the UHP event affected the whole stack of nappes and also that the pressures reached are above what was previously expected, since the presence of diamond, according to the peak temperature estimates for this unit, indicates pressures of ca. 3 GPa (i.e. 100 km depth). At the scale of the FMC, this finding adds complexity to the established models. On a broader scale, this adds evidence of similarity between this part of the belt and other UHP Variscan terranes such as the Erzgebirge and the Bohemian Massif |
2015Article de journal ER2 Auteurs : Thiéry, Vincent; Bourdot, Alexandra; Bulteel, David Characterization of raw and burnt oil shale from Dotternhausen: Petrographical and mineralogical evolution with temperature Dans: Materials Characterization, vol. 106, p. 442–451, 2015, (ACL). Liens @article{Thiery2015b,
title = {Characterization of raw and burnt oil shale from Dotternhausen: Petrographical and mineralogical evolution with temperature},
author = {Vincent Thiéry and Alexandra Bourdot and David Bulteel},
doi = {10.1016/j.matchar.2015.06.022},
year = {2015},
date = {2015-08-01},
journal = {Materials Characterization},
volume = {106},
pages = {442--451},
publisher = {Elsevier BV},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2014Manuel technique ER2 Auteurs : GATEL, P; ZACEK, V; KRUSZEWSKI, L; DEVOUARD, B; Thiery, Vincent; EYTIER, C; EYTIER, J-R; FAVREAU, G; VIGIER, J; GLENN, STRACHER B Combustion Mineralogy of Oil-Shale Slags, in ÂCoal and Peat Fires: A Global Perspective. Volume 3: Case Studies  Coal FiresÂ, Chapter 28, pp 682-742. Eds. G. Stracher, AṖrakash & E.V. So Elsevier, 2014, (OS). Résumé @manual{GATE2014A,
title = {Combustion Mineralogy of Oil-Shale Slags, in ÂCoal and Peat Fires: A Global Perspective. Volume 3: Case Studies  Coal FiresÂ, Chapter 28, pp 682-742. Eds. G. Stracher, AṖrakash & E.V. So},
author = {P GATEL and V ZACEK and L KRUSZEWSKI and B DEVOUARD and Vincent Thiery and C EYTIER and J-R EYTIER and G FAVREAU and J VIGIER and STRACHER B GLENN},
year = {2014},
date = {2014-00-01},
edition = {Elsevier},
abstract = {Coal and Peat Fires: A Global Perspective, Volumes 1-4, presents a fascinating collection of research about prehistoric and historic coal and peat fires. Magnificent illustrations of fires and research findings from countries around the world are featured-a totally new contribution to science. This third of four volumes in the collection, Coal Fires - Case Studies, examines in detail specific coal fires chronicled in a number of locations around the world including Brazil, the Czech Republic, Germany, Malawi, Poland, Russia, Spain, Tajikistan, the United States, Venezuela, and others.},
note = {OS},
keywords = {ER2},
pubstate = {published},
tppubtype = {manual}
}
Coal and Peat Fires: A Global Perspective, Volumes 1-4, presents a fascinating collection of research about prehistoric and historic coal and peat fires. Magnificent illustrations of fires and research findings from countries around the world are featured-a totally new contribution to science. This third of four volumes in the collection, Coal Fires - Case Studies, examines in detail specific coal fires chronicled in a number of locations around the world including Brazil, the Czech Republic, Germany, Malawi, Poland, Russia, Spain, Tajikistan, the United States, Venezuela, and others. |
2014Article de journal ER2 Auteurs : Moundoungou, I; Bulteel, David; Garcia-Diaz, E; Thiery, Vincent; é, P D; Hammerschlag, J G Reduction of ASR expansion in concretes based on reactive chert aggregates: Effect of alkali neutralisation capacity Dans: Construction and Building Materials, vol. 54, p. 147Â162, 2014, (ACL). Résumé | Liens @article{MOUN2014B,
title = {Reduction of ASR expansion in concretes based on reactive chert aggregates: Effect of alkali neutralisation capacity},
author = {I Moundoungou and David Bulteel and E Garcia-Diaz and Vincent Thiery and P D é and J G Hammerschlag},
doi = {doi.org/10.1016/j.conbuildmat.2013.12.036},
year = {2014},
date = {2014-03-01},
journal = {Construction and Building Materials},
volume = {54},
pages = {147Â162},
abstract = {Previous studies on concretes based on reactive chert aggregates recognised that for a fixed amount of alkali, there is a reactive silica content that induces maximal expansion due to the alkaliÂsilica reaction (ASR). Beyond this critical point called the ÂpessimumÂ, the ASR expansion decreases. The various theories proposed to explain this phenomenon are not all in agreement and do not explore sufficiently the possibility of using the pessimum effect for the implementation of concretes with low ASR expansion. The objective of the present work was to consider the reduction of ASR expansion according to a pessimum effect and its relationship with the evolution of local alkali contents in silica grain. An accelerated expansion test was performed at 60 °C and 100% relative humidity (RH) on the concrete mixture based on reactive chert aggregates. The relative longitudinal variations of the prisms (DL/L) were measured over 24 weeks and microstructural studies were conducted on the samples tested. The results showed that the increase in reactive aggregate proportion allowed the reduction of the alkaliÂsilica reaction (ASR) expansion. This expansion reduction, attributed to a pessimum effect, could be used to prevent risk of ASR expansion in the concretes made with potentially reactive aggregates. The phenomenon of reduction of the expansion was explained in this paper by the capacity of reactive siliceous phases in the aggregates to fix alkali ions up to a certain threshold without being degraded. This neutralising capacity was identified thanks to EDS analyses by monitoring the increasing of the height of alkali peaks according to the microstructural degradation. Indeed, at the microstructural scale, two area types were identified to be major in the less expansive mixture: 1/undegraded areas which predominate, showed no detection of sodium, potassium and calcium as it appeared for the raw materials (degree 0). 2/areas in which signs of low degradation appeared were characterised by a slight increasing of alkali signals (degree 1). In contrast, in expansive mixture the alkali signal intensities were higher for the most degraded zones (degrees 2 and 3). The neutralisation process, induced by mixing concrete with both coarse and fine chert aggregates, is so dominant that the Âlocal alkali threshold causing the reaction is rarely exceeded, and expansions are below the standard limit. In terms of application, knowledge of the alkali threshold may help to verify the effectiveness of fixing harmful alkalis in the granular skeleton and could allow optimising the future concrete mixtures.},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
Previous studies on concretes based on reactive chert aggregates recognised that for a fixed amount of alkali, there is a reactive silica content that induces maximal expansion due to the alkaliÂsilica reaction (ASR). Beyond this critical point called the ÂpessimumÂ, the ASR expansion decreases. The various theories proposed to explain this phenomenon are not all in agreement and do not explore sufficiently the possibility of using the pessimum effect for the implementation of concretes with low ASR expansion. The objective of the present work was to consider the reduction of ASR expansion according to a pessimum effect and its relationship with the evolution of local alkali contents in silica grain. An accelerated expansion test was performed at 60 °C and 100% relative humidity (RH) on the concrete mixture based on reactive chert aggregates. The relative longitudinal variations of the prisms (DL/L) were measured over 24 weeks and microstructural studies were conducted on the samples tested. The results showed that the increase in reactive aggregate proportion allowed the reduction of the alkaliÂsilica reaction (ASR) expansion. This expansion reduction, attributed to a pessimum effect, could be used to prevent risk of ASR expansion in the concretes made with potentially reactive aggregates. The phenomenon of reduction of the expansion was explained in this paper by the capacity of reactive siliceous phases in the aggregates to fix alkali ions up to a certain threshold without being degraded. This neutralising capacity was identified thanks to EDS analyses by monitoring the increasing of the height of alkali peaks according to the microstructural degradation. Indeed, at the microstructural scale, two area types were identified to be major in the less expansive mixture: 1/undegraded areas which predominate, showed no detection of sodium, potassium and calcium as it appeared for the raw materials (degree 0). 2/areas in which signs of low degradation appeared were characterised by a slight increasing of alkali signals (degree 1). In contrast, in expansive mixture the alkali signal intensities were higher for the most degraded zones (degrees 2 and 3). The neutralisation process, induced by mixing concrete with both coarse and fine chert aggregates, is so dominant that the Âlocal alkali threshold causing the reaction is rarely exceeded, and expansions are below the standard limit. In terms of application, knowledge of the alkali threshold may help to verify the effectiveness of fixing harmful alkalis in the granular skeleton and could allow optimising the future concrete mixtures. |
2014Article de journal ER2 Auteurs : SOKOL, E V; KOKH, S N; VAPNIK, Yevgeny; Thiery, Vincent; KHORZHOVA, Sophia Natural analogs of belite sulfoaluminate cement clinkers from Negev Đesert, Israel Dans: American Mineralogist, vol. 99, no. 7, p. 1471-1487, 2014, (ACL). Résumé | Liens @article{SOKO2014B,
title = {Natural analogs of belite sulfoaluminate cement clinkers from Negev Đesert, Israel},
author = {E V SOKOL and S N KOKH and Yevgeny VAPNIK and Vincent Thiery and Sophia KHORZHOVA},
doi = {10.2138/am.2014.4704},
year = {2014},
date = {2014-11-01},
journal = {American Mineralogist},
volume = {99},
number = {7},
pages = {1471-1487},
abstract = {YeÂelimite-larnite rocks in the Hatrurim formation of the Negev Desert, Israel, are natural analogs of belite sulfoaluminate (BSA) cement clinkers. They have been produced by ultrahigh-temperature combustion metamorphism at ambient pressure of a calcareous sedimentary precursor. Their mineralogy consists of 35Â50 vol% ?-Ca2SiO4, 15Â20 vol% yeÂelimite, 7Â15 vol% ferrites, and 15Â20 vol% fluorapatite and/or fluorellestadite. A few grains of hatrurite (Ca3SiO5) and ??-Ca2SiO4 have been observed as well. The composition of ??- and ?-Ca2SiO4 polymorphs by EPMA are near Ca1.96Â1.98Na0.01Â0.02 Si0.96P0.03Al0.01O4, whereas yeÂelimite has an approximate composition by EPMA of Ca3.99Mg0.02Ba0.01Na0.02K0.02Al5.73Fe3+0.16Si0.10S0.97P0.02O16. The Al content of brownmillerite Ca2(Fe1?xAlx)2O5 ranges from x = 0.20Â0.27. Fe-analog of shulamitite (Ca3Fe2TiO8) contains up to 15.1 wt% TiO2. YeÂelimite-larnite rocks were derived from chalky sediments by burning of combustible gas with a Tmax at 1200Â1350 °C. The mineral content, microstructure, and texture/fabric of the yeÂelimite-larnite rocks imply that chalky and/or marly sediments with randomly distributed clay, phosphorite, and gypsum may be utilized as cheap naturally homogenized and pulverized mixtures for industrial production of BSA cement clinker, as an environment-friendly alternative to ordinary Portland cement (OPC).},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
YeÂelimite-larnite rocks in the Hatrurim formation of the Negev Desert, Israel, are natural analogs of belite sulfoaluminate (BSA) cement clinkers. They have been produced by ultrahigh-temperature combustion metamorphism at ambient pressure of a calcareous sedimentary precursor. Their mineralogy consists of 35Â50 vol% ?-Ca2SiO4, 15Â20 vol% yeÂelimite, 7Â15 vol% ferrites, and 15Â20 vol% fluorapatite and/or fluorellestadite. A few grains of hatrurite (Ca3SiO5) and ??-Ca2SiO4 have been observed as well. The composition of ??- and ?-Ca2SiO4 polymorphs by EPMA are near Ca1.96Â1.98Na0.01Â0.02 Si0.96P0.03Al0.01O4, whereas yeÂelimite has an approximate composition by EPMA of Ca3.99Mg0.02Ba0.01Na0.02K0.02Al5.73Fe3+0.16Si0.10S0.97P0.02O16. The Al content of brownmillerite Ca2(Fe1?xAlx)2O5 ranges from x = 0.20Â0.27. Fe-analog of shulamitite (Ca3Fe2TiO8) contains up to 15.1 wt% TiO2. YeÂelimite-larnite rocks were derived from chalky sediments by burning of combustible gas with a Tmax at 1200Â1350 °C. The mineral content, microstructure, and texture/fabric of the yeÂelimite-larnite rocks imply that chalky and/or marly sediments with randomly distributed clay, phosphorite, and gypsum may be utilized as cheap naturally homogenized and pulverized mixtures for industrial production of BSA cement clinker, as an environment-friendly alternative to ordinary Portland cement (OPC). |
2014Article de journal ER2 Auteurs : Thiery, Vincent Le district minier et les anciennes mines d antimoine de Merinchal (Creuse) Dans: Le cahier des micromonteurs, vol. 123, no. 1, p. 1-8, 2014, (SCL). @article{THIE2014A,
title = {Le district minier et les anciennes mines d antimoine de Merinchal (Creuse)},
author = {Vincent Thiery},
year = {2014},
date = {2014-01-01},
journal = {Le cahier des micromonteurs},
volume = {123},
number = {1},
pages = {1-8},
note = {SCL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2014Article de journal ER2 Auteurs : Thiery, Vincent Characterization of fibrous mimetite Dans: Microscopy and Microanalysis, vol. 20, no. 2, p. 596-601, 2014, (ACL). @article{THIE2014B,
title = {Characterization of fibrous mimetite},
author = {Vincent Thiery},
year = {2014},
date = {2014-01-01},
journal = {Microscopy and Microanalysis},
volume = {20},
number = {2},
pages = {596-601},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2014Article de journal ER2 Auteurs : Thiery, Vincent La tourmaline des Lartault et Naudiots, Marmagne (Saône et Loire) Dans: Le r`egne minéral, no. 115, p. 41-42, 2014, (ACL). @article{THIE2014D,
title = {La tourmaline des Lartault et Naudiots, Marmagne (Saône et Loire)},
author = {Vincent Thiery},
year = {2014},
date = {2014-01-01},
journal = {Le r`egne minéral},
number = {115},
pages = {41-42},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2014Conférence ER2 Auteurs : Thiery, Vincent; Damidot, Denis; Sokol, E; Kokh, S-N Ħydration properties of natural cementitious phases bearing rocks 36th meeting of the International Cement Microscopy Association, Milano, 2014, (ACTI). @conference{THIE2014C,
title = {Ħydration properties of natural cementitious phases bearing rocks},
author = {Vincent Thiery and Denis Damidot and E Sokol and S-N Kokh},
year = {2014},
date = {2014-01-01},
booktitle = {36th meeting of the International Cement Microscopy Association},
address = {Milano},
note = {ACTI},
keywords = {ER2},
pubstate = {published},
tppubtype = {conference}
}
|
2013Article de journal ER4 Auteurs : Thiéry, Vincent; Sokol, Ella-V.; Kokh, Svetlana-N.; Masalehdani, M. -Naze-Nancy Le métamorphisme naturel d’ultra-haute température (UHT) des roches à Ca-Si (Al, Fe) - Comparaison avec la minéralogie du clinker Dans: Géochronique, vol. 126, p. 27-29, 2013, (ACLN). @article{Thiery2013,
title = {Le métamorphisme naturel d’ultra-haute température (UHT) des roches à Ca-Si (Al, Fe) - Comparaison avec la minéralogie du clinker},
author = {Vincent Thiéry and Ella-V. Sokol and Svetlana-N. Kokh and M.-Naze-Nancy Masalehdani},
year = {2013},
date = {2013-01-01},
journal = {Géochronique},
volume = {126},
pages = {27-29},
note = {ACLN},
keywords = {ER4},
pubstate = {published},
tppubtype = {article}
}
|
2013Article de journal ER4 Auteurs : Thiéry, Vincent; Vladimirovna-Sokol, Ellina; Masalehdani, M. -Naze-Nancy; Guy, Bernard La combustion des terrils Dans: Géochronique, vol. 127, p. 23-25, 2013, (ACLN). Résumé @article{Thiery2013a,
title = {La combustion des terrils},
author = {Vincent Thiéry and Ellina Vladimirovna-Sokol and M.-Naze-Nancy Masalehdani and Bernard Guy},
year = {2013},
date = {2013-01-01},
journal = {Géochronique},
volume = {127},
pages = {23-25},
abstract = {La combustion des terrils est une spécificité des régions où du charbon est (ou a été) exploité [nous ne présenterons pas ici la combustion des stériles d’autres exploitations (schistes bitumineux, …) ni de la combustion des résidus métallurgiques]. ce phénomène spectaculaire est relativement courant et suivi de près d’une part à cause des risques d’explosion qui lui sont liés et d'autre part à cause des conséquences environnementales. du point de vue du pétrographe, des paragénèses inhabituelles de ultra-haute température à pression ambiante se développent, ainsi que des efflorescences de minéraux complexes, donnant ainsi des opportunités pour leur étude.},
note = {ACLN},
keywords = {ER4},
pubstate = {published},
tppubtype = {article}
}
La combustion des terrils est une spécificité des régions où du charbon est (ou a été) exploité [nous ne présenterons pas ici la combustion des stériles d’autres exploitations (schistes bitumineux, …) ni de la combustion des résidus métallurgiques]. ce phénomène spectaculaire est relativement courant et suivi de près d’une part à cause des risques d’explosion qui lui sont liés et d'autre part à cause des conséquences environnementales. du point de vue du pétrographe, des paragénèses inhabituelles de ultra-haute température à pression ambiante se développent, ainsi que des efflorescences de minéraux complexes, donnant ainsi des opportunités pour leur étude. |
2013Conférence ER2 Auteurs : Bourdot, Alexandra; Thiery, Vincent; Bulteel, David Effects of spent shales on reactive aggregates based concrete toward alkali-silica reaction 14th Euroseminar of Microscopy Applied to Building Materials (EMABM), Helsingør, 2013. @conference{BOUR2013A,
title = {Effects of spent shales on reactive aggregates based concrete toward alkali-silica reaction},
author = {Alexandra Bourdot and Vincent Thiery and David Bulteel},
year = {2013},
date = {2013-01-01},
booktitle = {14th Euroseminar of Microscopy Applied to Building Materials (EMABM)},
pages = {21-24},
address = {Helsingør},
keywords = {ER2},
pubstate = {published},
tppubtype = {conference}
}
|
2013Article de journal ER2 Auteurs : Thiery, Vincent External and internal features of garnet revealed by the multifocusimaging technique, Micron, http://dx.doi.org/10.1016/j.micron.2012.06.006,vol 44, pp675-678 Dans: 2013, (ACL). @article{THIE2013A,
title = {External and internal features of garnet revealed by the multifocusimaging technique, Micron, http://dx.doi.org/10.1016/j.micron.2012.06.006,vol 44, pp675-678},
author = {Vincent Thiery},
year = {2013},
date = {2013-01-01},
note = {ACL},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2013Article de journal ER2 Auteurs : Thiery, Vincent Điversite des pratiques en laboratoires Dans: Mines & Carrieres, vol. 206, p. 174-176, 2013. @article{THIE2013B,
title = {Điversite des pratiques en laboratoires},
author = {Vincent Thiery},
year = {2013},
date = {2013-01-01},
journal = {Mines & Carrieres},
volume = {206},
pages = {174-176},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2013Article de journal ER2 Auteurs : Thiery, Vincent; Cartannaz, C Ŧhe Merinchal antimoniferous district (French Massif Central) Dans: Periodico di Mineralogia - Special issue: Mineral applications on Environments, Archaeometry and Cultural Heritage, vol. 82, no. 1, p. 129-140, 2013. @article{THIE2013C,
title = {Ŧhe Merinchal antimoniferous district (French Massif Central)},
author = {Vincent Thiery and C Cartannaz},
year = {2013},
date = {2013-01-01},
journal = {Periodico di Mineralogia - Special issue: Mineral applications on Environments, Archaeometry and Cultural Heritage},
volume = {82},
number = {1},
pages = {129-140},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2013Article de journal ER2 Auteurs : Thiery, Vincent; Sokol, Ella-V.; Kokh, Svetlana-N.; Masalehdani, M. -Naze-Nancy Le métamorphisme naturel à ultra-haute température (UHT) des roches `a Ca-Si (Al, Fe) - Comparaison avec la minéralogie du clink Dans: Géochronique, vol. 126, p. 27-29, 2013, (ACLN). @article{Thie2013e,
title = {Le métamorphisme naturel à ultra-haute température (UHT) des roches `a Ca-Si (Al, Fe) - Comparaison avec la minéralogie du clink},
author = {Vincent Thiery and Ella-V. Sokol and Svetlana-N. Kokh and M.-Naze-Nancy Masalehdani},
year = {2013},
date = {2013-01-01},
journal = {Géochronique},
volume = {126},
pages = {27-29},
note = {ACLN},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2013Article de journal ER2 Auteurs : Thiery, Vincent; Vladimirovna-Sokol, Ellina; Masalehdani, M. -Naze-Nancy; Guy, Bernard La combustion des terrils Dans: Géochronique, vol. 127, p. 23-25, 2013, (ACLN). Résumé @article{Thie2013d,
title = {La combustion des terrils},
author = {Vincent Thiery and Ellina Vladimirovna-Sokol and M.-Naze-Nancy Masalehdani and Bernard Guy},
year = {2013},
date = {2013-01-01},
journal = {Géochronique},
volume = {127},
pages = {23-25},
abstract = {La combustion des terrils est une spécificité des régions o`u du charbon est (ou a été) exploité [Nous ne présenterons pas ici la combustion des stériles dâautres exploitations (schistes bitumineux, â¦) ni de la combustion des résidus métallurgiques]. Ce phénom`ene spectaculaire est relativement courant et suivi de pr`es dâune part `a cause des risques dâexplosion qui lui sont liés et d'autre part `a cause des conséquences environnementales. Du point de vue du pétrographe, des paragén`eses inhabituelles de ultra-haute température `a pression ambiante se développent, ainsi que des efflorescences de minéraux complexes, donnant ainsi des opportunités pour leur étude.},
note = {ACLN},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
La combustion des terrils est une spécificité des régions o`u du charbon est (ou a été) exploité [Nous ne présenterons pas ici la combustion des stériles dâautres exploitations (schistes bitumineux, â¦) ni de la combustion des résidus métallurgiques]. Ce phénom`ene spectaculaire est relativement courant et suivi de pr`es dâune part `a cause des risques dâexplosion qui lui sont liés et d'autre part `a cause des conséquences environnementales. Du point de vue du pétrographe, des paragén`eses inhabituelles de ultra-haute température `a pression ambiante se développent, ainsi que des efflorescences de minéraux complexes, donnant ainsi des opportunités pour leur étude. |
2012Article de journal ER2 Auteurs : Thiery, Vincent La serie de la Sioule, 75 ans apres les travaux de J. Richard (1938) - Ħistorique des etudes geologiques et evolution des concepts Dans: Bulletin de la societe d histoire naturelle d Auvergne, vol. 76, p. 73-91, 2012. @article{THIE2012A,
title = {La serie de la Sioule, 75 ans apres les travaux de J. Richard (1938) - Ħistorique des etudes geologiques et evolution des concepts},
author = {Vincent Thiery},
year = {2012},
date = {2012-01-01},
journal = {Bulletin de la societe d histoire naturelle d Auvergne},
volume = {76},
pages = {73-91},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2012Article de journal ER2 Auteurs : Thiery, Vincent Ŧhe multifocus imaging technique in petrology Dans: Computers & Geosciences, vol. 45, p. 131-138, 2012. Liens @article{THIE2012B,
title = {Ŧhe multifocus imaging technique in petrology},
author = {Vincent Thiery},
doi = {0098-3004 doi: 10.1016/j.cageo.2011.10.027},
year = {2012},
date = {2012-01-01},
journal = {Computers & Geosciences},
volume = {45},
pages = {131-138},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2011Article de journal ER2 Auteurs : Thiery, Vincent Cumulative cordieritite formation as a result of anatexis and melt expulsion. An example from the Chavanon sequence, Variscan French Massif Central Dans: Periodico di Mineralogia, vol. 80, no. 2, p. 267-285, 2011. @article{THIE2011C,
title = {Cumulative cordieritite formation as a result of anatexis and melt expulsion. An example from the Chavanon sequence, Variscan French Massif Central},
author = {Vincent Thiery},
year = {2011},
date = {2011-01-01},
journal = {Periodico di Mineralogia},
volume = {80},
number = {2},
pages = {267-285},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2011Article de journal ER2 Auteurs : Thiery, Vincent Sur les pentes du Coupet (Ħaute-Loire) Dans: Le regne mineral, vol. 98, p. 28, 2011. @article{THIE2011D,
title = {Sur les pentes du Coupet (Ħaute-Loire)},
author = {Vincent Thiery},
year = {2011},
date = {2011-01-01},
journal = {Le regne mineral},
volume = {98},
pages = {28},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2011Ouvrage ER2 Auteurs : Thiery, Vincent; Rolin, P; Cocherie, A Notice explicative de la carte geologique dÚssel (n 667) 2011. @book{THIE2011E,
title = {Notice explicative de la carte geologique dÚssel (n 667)},
author = {Vincent Thiery and P Rolin and A Cocherie},
year = {2011},
date = {2011-01-01},
keywords = {ER2},
pubstate = {published},
tppubtype = {book}
}
|
2010Article de journal ER2 Auteurs : Lebocey, J; Thiery, Vincent; Gratia, B La concession miniere de Meymac (Correze) Dans: Le regne mineral, vol. 91, p. 9-22, 2010. @article{LEBO2010A,
title = {La concession miniere de Meymac (Correze)},
author = {J Lebocey and Vincent Thiery and B Gratia},
year = {2010},
date = {2010-01-01},
journal = {Le regne mineral},
volume = {91},
pages = {9-22},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
|
2010Ouvrage ER2 Auteurs : Thiery, Vincent Metamorphismes et deformations des series cristallophylliennes du Chavanon, de la Sioule et d Ussel (Massif Central francais). Điscussion du modele de nappes du Massif Central. PhḊ. Đissertation, Universite de Franche-Comte [in French] Besançon, France, 2010. @book{THIE2010A,
title = {Metamorphismes et deformations des series cristallophylliennes du Chavanon, de la Sioule et d Ussel (Massif Central francais). Điscussion du modele de nappes du Massif Central. PhḊ. Đissertation, Universite de Franche-Comte [in French]},
author = {Vincent Thiery},
year = {2010},
date = {2010-01-01},
address = {Besançon, France},
keywords = {ER2},
pubstate = {published},
tppubtype = {book}
}
|
2010Ouvrage ER2 Auteurs : Thiery, Vincent; Rolin, P; Barrau, F; Catimel, F; Choulet, F; Eglinger, A; Moreau, E; Belle, P; Boucly, J; Juppe, E; Lafay, R; Ravier, M; Reile, B Carte geologique de la France, feuille Ussel. Notice explicative par Ŧhiery, V., Rolin, P. et Cocherie, A., 169p 2010. @book{THIE2010B,
title = {Carte geologique de la France, feuille Ussel. Notice explicative par Ŧhiery, V., Rolin, P. et Cocherie, A., 169p},
author = {Vincent Thiery and P Rolin and F Barrau and F Catimel and F Choulet and A Eglinger and E Moreau and P Belle and J Boucly and E Juppe and R Lafay and M Ravier and B Reile},
year = {2010},
date = {2010-01-01},
keywords = {ER2},
pubstate = {published},
tppubtype = {book}
}
|
2009Article de journal ER2 Auteurs : Thiery, Vincent Famenno-Carboniferous (370-320 Ma) strike slip tectonics monitoredby syn-kinematic plutons in the French Variscan belt (Massif Armoricainand French Massif Central) Dans: Bulletin de la societe geologique de France, vol. 180, no. 3, p. 231-246, 2009. Résumé @article{ROLI2009A,
title = {Famenno-Carboniferous (370-320 Ma) strike slip tectonics monitoredby syn-kinematic plutons in the French Variscan belt (Massif Armoricainand French Massif Central)},
author = {Vincent Thiery},
year = {2009},
date = {2009-01-01},
journal = {Bulletin de la societe geologique de France},
volume = {180},
number = {3},
pages = {231-246},
abstract = {The Variscan continental collision has led to the development of large strike-slip shear zones in western Europe. Our study focuses on the regional deformation and shear zone patterns in the Massif Armoricain and the French Massif Central. The synthesis of granite emplacement ages associated to granite deformation fields, allow us to propose a geodynamic model for the tectonic evolution of this part of the Variscan belt between 370 Ma - 320 Ma (Late Devonian - Namurian). After the first steps of the continental subduction-collision, leading to high temperature and anatexis associated with N-S shortening at 380-370 Ma (Frasnian to Famennian), the southern part of the Massif Armoricain and western part of French Massif Central underwent large dextral shearing along N100-N130 trending shear zones up to early Visean time. These large-scale displacements progressively decreased at around 350-340 Ma, during the first emplacements of biotite bearing granites (Moulins-les Aubiers-Gourge massif and Gueret massif intrusions). During middle Visean times, the shortening axis direction rotated towards a NNE-SSW direction implying changes in the regional deformation field. The occurrence of N070-N100 sinistral and N110-N130 dextral conjugate shear zones within leucogranites are related to that time. Finally, new N150-N160 dextral shear zones appeared in middle to late Visean times: as for examples, the Parthenay and the Pradines shear zones in the SE Massif Armoricain and the Millevaches massif, respectively. These shear zones were conjugated to the sinistral N020 Sillon Houiller in the French Massif Central. They reflect large scale brittle continental indentation in the French Variscan belt during the middle to late Visean.},
keywords = {ER2},
pubstate = {published},
tppubtype = {article}
}
The Variscan continental collision has led to the development of large strike-slip shear zones in western Europe. Our study focuses on the regional deformation and shear zone patterns in the Massif Armoricain and the French Massif Central. The synthesis of granite emplacement ages associated to granite deformation fields, allow us to propose a geodynamic model for the tectonic evolution of this part of the Variscan belt between 370 Ma - 320 Ma (Late Devonian - Namurian). After the first steps of the continental subduction-collision, leading to high temperature and anatexis associated with N-S shortening at 380-370 Ma (Frasnian to Famennian), the southern part of the Massif Armoricain and western part of French Massif Central underwent large dextral shearing along N100-N130 trending shear zones up to early Visean time. These large-scale displacements progressively decreased at around 350-340 Ma, during the first emplacements of biotite bearing granites (Moulins-les Aubiers-Gourge massif and Gueret massif intrusions). During middle Visean times, the shortening axis direction rotated towards a NNE-SSW direction implying changes in the regional deformation field. The occurrence of N070-N100 sinistral and N110-N130 dextral conjugate shear zones within leucogranites are related to that time. Finally, new N150-N160 dextral shear zones appeared in middle to late Visean times: as for examples, the Parthenay and the Pradines shear zones in the SE Massif Armoricain and the Millevaches massif, respectively. These shear zones were conjugated to the sinistral N020 Sillon Houiller in the French Massif Central. They reflect large scale brittle continental indentation in the French Variscan belt during the middle to late Visean. |
