Faure, Michel, Sommers, Claire, Melleton, Jérémie, Cocherie, Alain, Lautout, Olivier
The Léon Domain in the NW part of the French Massif Armoricain is a stack of synmetamorphic nappes displaced from south to north in ductile conditions. From bottom to top, an orthogneissic basement...
Faure, Michel, Sommers, Claire, Melleton, Jérémie, Cocherie, Alain, Lautout, Olivier
The Léon Domain in the NW part of the French Massif Armoricain is a stack of synmetamorphic nappes displaced from south to north in ductile conditions. From bottom to top, an orthogneissic basement...
A review of the pre-Permian geology of the Variscan French Massif Central (2009)
Faure, Michel, Lardeaux, Jean-Marc, Ledru, P.
The Massif Central, like the southern part of the Massif Armoricain, belongs to the North Gondwana margin. The Massif Central consists of a stack of nappes resulting of six main tectonic-metamorphic...
A review of the pre-Permian geology of the Variscan French Massif Central (2009)
Faure, Michel, Lardeaux, Jean-Marc, Ledru, P.
The Massif Central, like the southern part of the Massif Armoricain, belongs to the North Gondwana margin. The Massif Central consists of a stack of nappes resulting of six main tectonic-metamorphic...
Joly, Aurore, Faure, Michel, Martelet, Guillaume, Chen, Yan
Magnetic fabric analyses, gravity inversion associated with chemical U-Th-Pb dating and structural observations are carried out to elucidate relationships between faulting and magmatic processes....
Joly, Aurore, Faure, Michel, Martelet, Guillaume, Chen, Yan
Magnetic fabric analyses, gravity inversion associated with chemical U-Th-Pb dating and structural observations are carried out to elucidate relationships between faulting and magmatic processes....
Wang, Bo, Cluzel, Dominique, Shu, Liangshu S., Faure, Michel, Charvet, Jacques, Chen, Yan, ...
Continuous magmatic activity occurred in the western Chinese Tianshan, Central Asia, from the Carboniferous to the Permian, i.e. before and after the Late Carboniferous amalgamation of Junggar and...
Wang, Bo, Cluzel, Dominique, Shu, Liangshu S., Faure, Michel, Charvet, Jacques, Chen, Yan, ...
Continuous magmatic activity occurred in the western Chinese Tianshan, Central Asia, from the Carboniferous to the Permian, i.e. before and after the Late Carboniferous amalgamation of Junggar and...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick, Meffre, Sébastien, Melleton, Jérémie
This paper presents a reappraisal of the tectonic evolution of the Zanhuang Massif that lies at the eastern margin of the Trans-North China Orogen, a continent–continent collision belt that marked...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick, Meffre, Sébastien, Melleton, Jérémie
This paper presents a reappraisal of the tectonic evolution of the Zanhuang Massif that lies at the eastern margin of the Trans-North China Orogen, a continent–continent collision belt that marked...
Charles, Nicolas, Faure, Michel, Chen, Yan
In the southern French Massif Central, the Montagne Noire axial zone is a NE-SW elongated granite-migmatite dome emplaced within Visean south-verging recumbent folds and intruded by syn- to...
Charles, Nicolas, Faure, Michel, Chen, Yan
In the southern French Massif Central, the Montagne Noire axial zone is a NE-SW elongated granite-migmatite dome emplaced within Visean south-verging recumbent folds and intruded by syn- to...
Lin, Wei, Faure, Michel, Nomade, Sébastien, Shang, Qinghua, Randall Renne, Paul
The Central Asia Orogenic Belt (CAOB) corresponds to the domain where Siberia and Mongolia were welded to North China. The eastern extension of the CAOB in Northeast China is disputed, since both...
Lin, Wei, Faure, Michel, Nomade, Sébastien, Shang, Qinghua, Randall Renne, Paul
The Central Asia Orogenic Belt (CAOB) corresponds to the domain where Siberia and Mongolia were welded to North China. The eastern extension of the CAOB in Northeast China is disputed, since both...
Faure, Michel, Lin, Wei, Monié, Patrick, Meffre, Sébastien
The QinlingDabie Belt represents the boundary between the North and South China Blocks (NCB, SCB, respectively), where ultrahigh-pressure (UHP) rocks are widespread. A structural study in eastern...
Shu, Liangshu S., Faure, Michel, Wang, Bo, Zhou, Xinmin, Song, Biao
This paper provides some new evidences on stratigraphic sequence, zircon SHRIMP dating from ophiolite, granitoids, and fold-and-thrust tectonic styles in the South China Block (SCB). Stratigraphic...
Shu, Liangshu S., Faure, Michel, Wang, Bo, Zhou, Xinmin, Song, Biao
This paper provides some new evidences on stratigraphic sequence, zircon SHRIMP dating from ophiolite, granitoids, and fold-and-thrust tectonic styles in the South China Block (SCB). Stratigraphic...
Faure, Michel, Lin, Wei, Monié, Patrick, Meffre, Sébastien
The QinlingDabie Belt represents the boundary between the North and South China Blocks (NCB, SCB, respectively), where ultrahigh-pressure (UHP) rocks are widespread. A structural study in eastern...
Lin, Wei, Faure, Michel, Nomade, Sébastien, Shang, Qinghua, Randall Renne, Paul
The Central Asia Orogenic Belt (CAOB) corresponds to the domain where Siberia and Mongolia were welded to North China. The eastern extension of the CAOB in NE China is disputed, since both suture...
Lin, Wei, Faure, Michel, Nomade, Sébastien, Shang, Qinghua, Randall Renne, Paul
The Central Asia Orogenic Belt (CAOB) corresponds to the domain where Siberia and Mongolia were welded to North China. The eastern extension of the CAOB in NE China is disputed, since both suture...
Joly, Aurore, Martelet, Guillaume, Chen, Yan, Faure, Michel
New gravity and aeromagnetic investigations have been carried out to understand the emplacement mechanisms of a granitic pluton and the relationships with a nearby lithospheric-scale fault. This...
Joly, Aurore, Martelet, Guillaume, Chen, Yan, Faure, Michel
New gravity and aeromagnetic investigations have been carried out to understand the emplacement mechanisms of a granitic pluton and the relationships with a nearby lithospheric-scale fault. This...
Trap, Pierre, Faure, Michel, Lin, Wei, Bruguier, Olivier, Monié, Patrick
Structural analysis along with 40Ar–39Ar and U–Pb datings in the Fuping massif provide new insight into the evolution of the eastern part of the Trans-North China Belt (North China Craton), from...
Trap, Pierre, Faure, Michel, Lin, Wei, Bruguier, Olivier, Monié, Patrick
Structural analysis along with 40Ar39Ar and UPb datings in the Fuping massif provide new insight into the evolution of the eastern part of the Trans-North China Belt (North China Craton), from...
De Jong, Koenraad, Wang, Bo, Faure, Michel, Shu, Liangshu S., Cluzel, Dominique, Charvet, Jacques, ...
Laser-probe dating of mylonite whole-rock samples from the North Tianshan—Main Tianshan fault zone that cross-cuts the North Tianshan domain’s southern margin yielded 40Ar/39Ar spectra with...
De Jong, Koenraad, Wang, Bo, Faure, Michel, Shu, Liangshu S., Cluzel, Dominique, Charvet, Jacques, ...
Laser-probe dating of mylonite whole-rock samples from the North TianshanMain Tianshan fault zone that cross-cuts the North Tianshan domains southern margin yielded 40Ar/39Ar spectra with...
Faure, Michel, Be Mezeme, Eugène, Cocherie, Alain, Rossi, Ph., Chemenda, Alexandre, Boutelier, David
The Paleozoic French Variscan Belt in Massif Central and Massif Armoricain is a collision belt that provides a good example of a suture zone where ophiolites are rare, and the frontal (i.e., the...
Faure, Michel, Be Mezeme, Eugène, Cocherie, Alain, Rossi, Ph., Chemenda, Alexandre, Boutelier, David
The Paleozoic French Variscan Belt in Massif Central and Massif Armoricain is a collision belt that provides a good example of a suture zone where ophiolites are rare, and the frontal (i.e., the...
Lin, Wei, Faure, Michel, Monié, Patrick, Schärer, Urs, Panis, Dominique
In the North China block, the south Liaodong Peninsula massif is an elliptical metamorphic core complex (MCC) with a long axis trending NE‐SW. In cross‐section view, it is asymmetric, with a...
Lin, Wei, Faure, Michel, Monié, Patrick, Schärer, Urs, Panis, Dominique
In the North China block, the south Liaodong Peninsula massif is an elliptical metamorphic core complex (MCC) with a long axis trending NE‐SW. In cross‐section view, it is asymmetric, with a...
Wang, Bo, Shu, Liangshu S., Cluzel, Dominique, Faure, Michel, Charvet, Jacques
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic...
Zhan, Sheng, Chen, Yan, Xu, Bei, Wang, Bo, Faure, Michel
In order to better constrain the Neoproterozoic paleogeographic reconstruction of continents and to improve the understanding of the snowball Earth hypothesis, paleomagnetic investigations were...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick
The HengshanWutaishan area forms part of the Trans-North-China Belt developed in response to the final amalgamation of the North China Craton. The HengshanWutaishan domain and the adjacent Fuping...
Duguet, Manuel, Le Breton, Nicole, Faure, Michel
Because of late metamorphic and tectonic overprints, the reconstruction of prograde parts of PT paths is often difficult. In the SW Variscan French Massif Central, the Thiviers-Payzac Unit (TPU) is...
Wang, Bo, Chen, Yan, Zhan, Sheng, Shua, Liangshu, Faure, Michel, Cluzel, Dominique, ...
In order to better understand the tectonic role of the Yili Block on the Paleozoic evolution of the Chinese Tianshan Belt, we performed a primary paleomagnetic study on Carboniferous and Permian...
Lin, Wei, Enami, M., Faure, Michel, Schärer, Urs, Arnaud, Nicolas
Investigation of an eclogite xenolith, discovered in a Cretaceous granite from the Central Domain of the Dabieshan massif in eastern China, yields new petrological insights into the high to...
Lin, Wei, Enami, M., Faure, Michel, Schärer, Urs, Arnaud, Nicolas
Investigation of an eclogite xenolith, discovered in a Cretaceous granite from the Central Domain of the Dabieshan massif in eastern China, yields new petrological insights into the high to...
Wang, Bo, Chen, Yan, Zhan, Sheng, Shua, Liangshu, Faure, Michel, Cluzel, Dominique, ...
In order to better understand the tectonic role of the Yili Block on the Paleozoic evolution of the Chinese Tianshan Belt, we performed a primary paleomagnetic study on Carboniferous and Permian...
Duguet, Manuel, Le Breton, Nicole, Faure, Michel
Because of late metamorphic and tectonic overprints, the reconstruction of prograde parts of PT paths is often difficult. In the SW Variscan French Massif Central, the Thiviers-Payzac Unit (TPU) is...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick
The HengshanWutaishan area forms part of the Trans-North-China Belt developed in response to the final amalgamation of the North China Craton. The HengshanWutaishan domain and the adjacent Fuping...
Zhan, Sheng, Chen, Yan, Xu, Bei, Wang, Bo, Faure, Michel
In order to better constrain the Neoproterozoic paleogeographic reconstruction of continents and to improve the understanding of the snowball Earth hypothesis, paleomagnetic investigations were...
Wang, Bo, Shu, Liangshu S., Cluzel, Dominique, Faure, Michel, Charvet, Jacques
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic...
Chen, Yan, Henry, Bernard, Faure, Michel, Becq-Giraudon, Jean-François, Talbot, Jean-Yves, Daly, Lucien, ...
In order to assess the structural evolution of the Brive basin and the Paleozoic activity of surrounding major faults in the French Massif Central, we carried out a paleomagnetic study on Early...
Be Mezeme, Eugène, Cocherie, A., Faure, Michel, Lengendre, O., Rossi, Ph.
UThPb dating of monazite with the electron probe microanalyser (EPMA) is increasingly documented as a reliable geochronological method offering high spatial resolution. This method has been...
Tectonic evolution of the northern part of Western Tianshan (Xinjiang, NW China). (2006)
Wang, Bo, Shu, L.S., Cluzel, Dominique, Faure, Michel, Charvet, Jacques
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier, Le Breton, Nicole
In the North China Craton, the Paleoproterozoic Trans-North China Belt (TNCB) is a nearly north-south trending zone, of 1200 km long and 300 km wide, that separates two Archean blocks. Previous...
Vidal, Max, Trap, Pierre, Faure, Michel
L'évolution géodynamique au Paléoprotérozoïque reste un sujet débattu, les raisons principales étant le manque de datations, les différences d'interprétations structurale, et l'imprécision...
Trap, Pierre, Faure, Michel, Lin, Wei, Lebreton, Nicole, Bruguier, Olivier, Monié, Patrick
The Paleoproterozoic Trans-North China Belt is a nearly north-south trending zone, of 1000 km long and 300 km wide, which resulted from collision between two Archean Eastern and Western Blocks,...
L'évolution géodynamique de la chaîne paléozoïque du Tianshan (2006)
Faure, Michel, Wang, Bo, Cluzel, Dominique, Shu, Liangshu S., Charvet, Jacques, De Jong, Koenraad, ...
La chaîne du Tianshan s'étend sur plus de 3000 km en Asie centrale, elle sépare le Tarim au Sud du Juggar et du Kazakhstan au Nord (Fig. 1a). La collision indienne est responsable du haut-relief...
L'évolution géodynamique de la chaîne paléozoïque du Tianshan (2006)
Faure, Michel, Wang, Bo, Cluzel, Dominique, Shu, Liangshu S., Charvet, Jacques, De Jong, Koenraad, ...
La chaîne du Tianshan s'étend sur plus de 3000 km en Asie centrale, elle sépare le Tarim au Sud du Juggar et du Kazakhstan au Nord (Fig. 1a). La collision indienne est responsable du haut-relief...
Trap, Pierre, Faure, Michel, Lin, Wei, Lebreton, Nicole, Bruguier, Olivier, Monié, Patrick
The Paleoproterozoic Trans-North China Belt is a nearly north-south trending zone, of 1000 km long and 300 km wide, which resulted from collision between two Archean Eastern and Western Blocks,...
Vidal, Max, Trap, Pierre, Faure, Michel
L'évolution géodynamique au Paléoprotérozoïque reste un sujet débattu, les raisons principales étant le manque de datations, les différences d'interprétations structurale, et l'imprécision...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier, Le Breton, Nicole
In the North China Craton, the Paleoproterozoic Trans-North China Belt (TNCB) is a nearly north-south trending zone, of 1200 km long and 300 km wide, that separates two Archean blocks. Previous...
Chen, Yan, Henry, Bernard, Faure, Michel, Becq-Giraudon, Jean-François, Talbot, Jean-Yves, Daly, Lucien, ...
In order to assess the structural evolution of the Brive basin and the Paleozoic activity of surrounding major faults in the French Massif Central, we carried out a paleomagnetic study on Early...
Be Mezeme, Eugène, Cocherie, A., Faure, Michel, Lengendre, O., Rossi, Ph.
UThPb dating of monazite with the electron probe microanalyser (EPMA) is increasingly documented as a reliable geochronological method offering high spatial resolution. This method has been...
Tectonic evolution of the northern part of Western Tianshan (Xinjiang, NW China). (2006)
Wang, Bo, Shu, Liangshu S., Cluzel, Dominique, Faure, Michel, Charvet, Jacques
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic...
L'évolution géodynamique de la chaîne paléozoïque du Tianshan (2006)
Faure, Michel, Wang, Bo, Cluzel, Dominique, Shu, Liangshu S., Charvet, Jacques, De Jong, Koenraad, ...
La chaîne du Tianshan s'étend sur plus de 3000 km en Asie centrale, elle sépare le Tarim au Sud du Juggar et du Kazakhstan au Nord (Fig. 1a). La collision indienne est responsable du haut-relief...
Trap, Pierre, Faure, Michel, Lin, Wei, Le Breton, Nicole, Bruguier, Olivier, Monié, Patrick
The Paleoproterozoic Trans-North China Belt is a nearly north-south trending zone, of 1000 km long and 300 km wide, which resulted from collision between two Archean Eastern and Western Blocks,...
Vidal, Max, Trap, Pierre, Faure, Michel
L'évolution géodynamique au Paléoprotérozoïque reste un sujet débattu, les raisons principales étant le manque de datations, les différences d'interprétations structurale, et l'imprécision...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier, Le Breton, Nicole
In the North China Craton, the Paleoproterozoic Trans-North China Belt (TNCB) is a nearly north-south trending zone, of 1200 km long and 300 km wide, that separates two Archean blocks. Previous...
Chen, Yan, Henry, Bernard, Faure, Michel, Becq-Giraudon, Jean-François, Talbot, Jean-Yves, Daly, Lucien, ...
In order to assess the structural evolution of the Brive basin and the Paleozoic activity of surrounding major faults in the French Massif Central, we carried out a paleomagnetic study on Early...
Be Mezeme, Eugène, Cocherie, Alain, Faure, Michel, Lengendre, O., Rossi, Ph.
UThPb dating of monazite with the electron probe microanalyser (EPMA) is increasingly documented as a reliable geochronological method offering high spatial resolution. This method has been...
Tectonic evolution of the northern part of Western Tianshan (Xinjiang, NW China). (2006)
Wang, Bo, Shu, Liangshu S., Cluzel, Dominique, Faure, Michel, Charvet, Jacques
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic...
Gébelin, Aude, Martelet, Guillaume, Chen, Yan, Brunel, M., Faure, Michel
In the Limousin area, Variscan leucogranitic plutons are spatially associated with normal faults and major strike-slip shear zones that are a continuation of the South Armorican shear zone. Our study...
Be Mezeme, Eugène, Faure, Michel, Chen, Yan, Cocherie, Alain, Talbot, Jean-Yves
In the southern French Massif Central, the Rocles leucogranite of Variscan age consists of three petrographic facies; textural analysis shows that they experienced the same subsolidus deformation....
Vidal, Max, Trap, Pierre, Faure, Michel
Lévolution géodynamique au Paléoprotérozoïque reste un sujet débattu, les raisons principales étant le manque de datations, les différences dinterprétations structurale, et...
Trap, Pierre, Faure, Michel, Lin, Wei, Le Breton, Nicole, Bruguier, Olivier, Monié, Patrick
The Paleoproterozoic Trans-North China Belt is a nearly north-south trending zone, of 1000 km long and 300 km wide, which resulted from collision between two Archean Eastern and Western Blocks,...
Vidal, Max, Trap, Pierre, Faure, Michel
Lévolution géodynamique au Paléoprotérozoïque reste un sujet débattu, les raisons principales étant le manque de datations, les différences dinterprétations structurale, et...
Be Mezeme, Eugène, Cocherie, Alain, Faure, Michel, Lengendre, O., Rossi, Ph.
UThPb dating of monazite with the electron probe microanalyser (EPMA) is increasingly documented as a reliable geochronological method offering high spatial resolution. This method has been...
Be Mezeme, Eugène, Faure, Michel, Chen, Yan, Cocherie, Alain, Talbot, Jean-Yves
In the southern French Massif Central, the Rocles leucogranite of Variscan age consists of three petrographic facies; textural analysis shows that they experienced the same subsolidus deformation....
Gébelin, Aude, Martelet, Guillaume, Chen, Yan, Brunel, M., Faure, Michel
In the Limousin area, Variscan leucogranitic plutons are spatially associated with normal faults and major strike-slip shear zones that are a continuation of the South Armorican shear zone. Our study...
L'évolution géodynamique de la chaîne paléozoïque du Tianshan (2006)
Faure, Michel, Wang, Bo, Cluzel, Dominique, Shu, Liangshu S., Charvet, Jacques, De Jong, Koenraad, ...
La chaîne du Tianshan s'étend sur plus de 3000 km en Asie centrale, elle sépare le Tarim au Sud du Juggar et du Kazakhstan au Nord (Fig. 1a). La collision indienne est responsable du haut-relief...
Tectonic evolution of the northern part of Western Tianshan (Xinjiang, NW China). (2006)
Wang, Bo, Shu, Liangshu S., Cluzel, Dominique, Faure, Michel, Charvet, Jacques
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic...
Vidal, Max, Trap, Pierre, Faure, Michel
L'évolution géodynamique au Paléoprotérozoïque reste un sujet débattu, les raisons principales étant le manque de datations, les différences d'interprétations structurale, et l'imprécision...
Trap, Pierre, Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier, Le Breton, Nicole
In the North China Craton, the Paleoproterozoic Trans-North China Belt (TNCB) is a nearly north-south trending zone, of 1200 km long and 300 km wide, that separates two Archean blocks. Previous...
Chen, Yan, Henry, Bernard, Faure, Michel, Becq-Giraudon, Jean-François, Talbot, Jean-Yves, Daly, Lucien, ...
In order to assess the structural evolution of the Brive basin and the Paleozoic activity of surrounding major faults in the French Massif Central, we carried out a paleomagnetic study on Early...
In situ chemical dating of tectonothermal events in the French Variscan Belt. (2005)
Be Mezeme, Eugène, Faure, Michel, Cocherie, Alain, Chen, Yan
In situ UThPb geochronology on monazite using Electron Probe Micro Analyser has been performed on migmatite in the southern French Variscan Massif Central in order to decipher its complex...
Cocherie, Alain, Be Mezeme, Eugène, Legendre, Olivier, Fanning, C. Mark, Faure, Michel, Rossi, Philippe
High spatial resolution dating of monazite by the electron-probe microanalyzer (EPMA) enables systematic and detailed studies of small minerals. Like zircon, monazite records the complex history...
Talbot, Jean-Yves, Chen, Yan, Faure, Michel
In the southeastern French Massif Central, the AigoualSaint GuiralLiron pluton consists of porphyritic and microgranitic types. The latter is encountered within dikes forming the northern end of...
Talbot, Jean-Yves, Faure, Michel, Chen, Yan, Martelet, Guillaume
A microstructural, magnetic fabric and gravity study is performed on the Carboniferous Margeride granitic complex that crops out in the central part of the Variscan French Massif Central. This...
Late Paleozoic tectonic and magmatic evolution of the Chinese West Tianshan (2005)
Wang, Bo, Faure, Michel, Shu, Liangshu S., Cluzel, Dominique, Charvet, Jacques
In Xinjiang Province of NW China, the Tianshan Belt belongs to the Late Paleozoic Variscan orogens that shaped up the Eurasian continent. Most of geologists drew to a conclusion that the Tianshan...
Late Paleozoic tectonic and magmatic evolution of the Chinese West Tianshan (2005)
Wang, Bo, Faure, Michel, Shu, Liangshu S., Cluzel, Dominique, Charvet, Jacques
In Xinjiang Province of NW China, the Tianshan Belt belongs to the Late Paleozoic Variscan orogens that shaped up the Eurasian continent. Most of geologists drew to a conclusion that the Tianshan...
Talbot, Jean-Yves, Faure, Michel, Chen, Yan, Martelet, Guillaume
A microstructural, magnetic fabric and gravity study is performed on the Carboniferous Margeride granitic complex that crops out in the central part of the Variscan French Massif Central. This...
Late Paleozoic tectonic and magmatic evolution of the Chinese West Tianshan (2005)
Wang, Bo, Faure, Michel, Shu, Liangshu S., Cluzel, Dominique, Charvet, Jacques
In Xinjiang Province of NW China, the Tianshan Belt belongs to the Late Paleozoic Variscan orogens that shaped up the Eurasian continent. Most of geologists drew to a conclusion that the Tianshan...
Talbot, Jean-Yves, Faure, Michel, Chen, Yan, Martelet, Guillaume
A microstructural, magnetic fabric and gravity study is performed on the Carboniferous Margeride granitic complex that crops out in the central part of the Variscan French Massif Central. This...
Lin, Wei, Faure, Michel, Wang, Qingchen, Panis, Dominique, Monié, Patrick
The Feidong-Zhangbaling Massif is located between the Dabieshan and Sulu areas along the Tan-Lu fault in eastern China. Five tectonic-metamorphic events are distinguished there. The earliest...
Lin, Wei, Faure, Michel, Wang, Qingchen, Panis, Dominique, Monié, Patrick
The Feidong-Zhangbaling Massif is located between the Dabieshan and Sulu areas along the Tan-Lu fault in eastern China. Five tectonic-metamorphic events are distinguished there. The earliest...
Late Paleozoic tectonic and magmatic evolution of the Chinese West Tianshan (2005)
Wang, Bo, Faure, Michel, Shu, Liangshu S., Cluzel, Dominique, Charvet, Jacques
In Xinjiang Province of NW China, the Tianshan Belt belongs to the Late Paleozoic Variscan orogens that shaped up the Eurasian continent. Most of geologists drew to a conclusion that the Tianshan...
Talbot, Jean-Yves, Faure, Michel, Chen, Yan, Martelet, Guillaume
A microstructural, magnetic fabric and gravity study is performed on the Carboniferous Margeride granitic complex that crops out in the central part of the Variscan French Massif Central. This...
Gébelin, Aude, Martelet, Guillaume, Faure, Michel, Rossi, Philippe
The Millevaches granitic complex, located in the northern part of the French Massif Central, is elongated in a N-S direction, perpendicular to the main E-W trend of the Hercynian belt. It is affected...
n the French Massif Central, the RouergueAlbigeois area consists of three tectonic units stacked during the Hercynian orogeny. The structural analysis of the units and particularly the quartz left...
In the French Massif Central, the Devonian-Carboniferous tectonic evolution of the Rouergue-Albigeois area is characterized by three phases of low-angle ductile shearing. The first event D1, which...
Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier
n the north-eastern part of the North China Block, a mafic magmatic belt consisting of maficultramafic rocks and marine sedimentary rocks crops out between the northern Archean Anshan Block and a...
Talbot, Jean-Yves, Martelet, Guillaume, Courrioux, Gabriel, Chen, Yan, Faure, Michel
The emplacement mode and setting of the Late Hercynian Mont LozèreBorne granitic complex (French Massif Central), which consists of several plutons, is investigated. Structural and anisotropy of...
Chauvet, Alain, Onézime, Jérôme, Charvet, Jacques, Barbanson, Luc, Faure, Michel
In deformed massive sulfide deposits, it is commonly difficult to distinguish between primary stockwork mineralization and remobilized sulfides that occupy late cleavages and deformation structures,...
Cartier, Carine, Faure, Michel
In the southern part of the French Armorican massif, the Ligerian domain is located along the boundary between Gondwana and Armorica. Lithological, geochemical and structural data on the...
Palaeoproterozoic arc magnatism and collision in Liaodong Peninsula (north-east China). (2004)
Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier
In the north-eastern part of the North China Block, a afic magmatic belt consisting of maficultramafic rocks and marine sedimentary rocks crops out between the northern Archean Anshan Block and a...
Talbot, Jean-Yves, Martelet, Guillaume, Courrioux, Gabriel, Chen, Yan, Faure, Michel
The emplacement mode and setting of the Late Hercynian Mont LozèreBorne granitic complex (French Massif Central), which consists of several plutons, is investigated. Structural and anisotropy of...
Palaeoproterozoic arc magnatism and collision in Liaodong Peninsula (north-east China). (2004)
Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier
In the north-eastern part of the North China Block, a afic magmatic belt consisting of maficultramafic rocks and marine sedimentary rocks crops out between the northern Archean Anshan Block and a...
n the French Massif Central, the RouergueAlbigeois area consists of three tectonic units stacked during the Hercynian orogeny. The structural analysis of the units and particularly the quartz left...
Talbot, Jean-Yves, Martelet, Guillaume, Courrioux, Gabriel, Chen, Yan, Faure, Michel
The emplacement mode and setting of the Late Hercynian Mont LozèreBorne granitic complex (French Massif Central), which consists of several plutons, is investigated. Structural and anisotropy of...
Palaeoproterozoic arc magnatism and collision in Liaodong Peninsula (north-east China). (2004)
Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier
In the north-eastern part of the North China Block, a afic magmatic belt consisting of maficultramafic rocks and marine sedimentary rocks crops out between the northern Archean Anshan Block and a...
n the French Massif Central, the RouergueAlbigeois area consists of three tectonic units stacked during the Hercynian orogeny. The structural analysis of the units and particularly the quartz left...
Cartier, Carine, Faure, Michel
In the southern part of the French Armorican massif, the Ligerian domain is located along the boundary between Gondwana and Armorica. Lithological, geochemical and structural data on the...
Cartier, Carine, Faure, Michel
In the southern part of the French Armorican massif, the Ligerian domain is located along the boundary between Gondwana and Armorica. Lithological, geochemical and structural data on the...
Talbot, Jean-Yves, Martelet, Guillaume, Courrioux, Gabriel, Chen, Yan, Faure, Michel
The emplacement mode and setting of the Late Hercynian Mont LozèreBorne granitic complex (French Massif Central), which consists of several plutons, is investigated. Structural and anisotropy of...
Palaeoproterozoic arc magnatism and collision in Liaodong Peninsula (north-east China). (2004)
Faure, Michel, Lin, Wei, Monié, Patrick, Bruguier, Olivier
In the north-eastern part of the North China Block, a afic magmatic belt consisting of maficultramafic rocks and marine sedimentary rocks crops out between the northern Archean Anshan Block and a...
n the French Massif Central, the RouergueAlbigeois area consists of three tectonic units stacked during the Hercynian orogeny. The structural analysis of the units and particularly the quartz left...
Lin, Wei, Chen, Yan, Faure, Michel, Wang, Qingchen
A paleomagnetic study has been carried out in the east of the Tan-Lu fault, in Liaoning Province, NE China, to understand the timing of Tan-Lu fault activity. Samples aging from Early Paleozoic to...
Onézime, Jérôme, Charvet, Jacques, Faure, Michel, Bourdier, Jean-Louis, Chauvet, Alain
The South Portuguese Zone (SPZ) constitutes the southernmost segment of the Variscan Iberian Massif. It is bounded to the north by the Beja-Acebuches Ophiolitic Complex and related accretionary...
Faure, Michel, Lin, Wei, Schärer, Urs, Shu, Liangshu, Sun, Yan, Arnaud, Nicolas
In the Dabieshan, the available models for exhumation of ultrahigh-pressure (UHP) rocks are poorly constrained by structural data. A comprehensive structural and kinematic map and a general...
Talbot, Jean-Yves, Chen, Yan, Faure, Michel
The relationships between plutons and dykes of granite have been the topic of many studies since the hypothesis of "dyke propagation" was proposed as the main mode of ascent and emplacement of...
Talbot, Jean-Yves, Chen, Yan, Faure, Michel
The relationships between plutons and dykes of granite have been the topic of many studies since the hypothesis of "dyke propagation" was proposed as the main mode of ascent and emplacement of...
Talbot, Jean-Yves, Chen, Yan, Faure, Michel
The relationships between plutons and dykes of granite have been the topic of many studies since the hypothesis of "dyke propagation" was proposed as the main mode of ascent and emplacement of...
Talbot, Jean-Yves, Chen, Yan, Faure, Michel
The relationships between plutons and dykes of granite have been the topic of many studies since the hypothesis of "dyke propagation" was proposed as the main mode of ascent and emplacement of...
Cartier, Carine, Faure, Michel, Lardeux, H.
In spite of numerous studies, the geodynamic evolution of the Hercynian Orogeny of Western Europe is still controversial. In a recent paper, Shelley and Bossière (2000) propose that the Hercynian...
Cartier, Carine, Faure, Michel, Lardeux, H.
In spite of numerous studies, the geodynamic evolution of the Hercynian Orogeny of Western Europe is still controversial. In a recent paper, Shelley and Bossière (2000) propose that the Hercynian...
Where is the North ChinaSouth China block boundary in eastern China? (2001)
Faure, Michel, Lin, Wei, Le Breton, Nicole
The Qinling-Dabieshan belt results from the collision of the North China and South China blocks. The eastern extension of the belt (the Sulu area) consists of several stacked units: from top to...
Lin, Wei, Faure, Michel, Sun, Yan, Shu, Liangshu S., Wang, Qingchen
The Jiulingshan massif is an EW trending anticlinorium in the South China Block (SCB) that forms the southern foreland of the QinlingDabie orogen. The Jiulingshan consists of Middle Proterozoic...
Lin, Wei, Faure, Michel, Sun, Yan, Shu, Liangshu S., Wang, Qingchen
The Jiulingshan massif is an EW trending anticlinorium in the South China Block (SCB) that forms the southern foreland of the QinlingDabie orogen. The Jiulingshan consists of Middle Proterozoic...
Where is the North ChinaSouth China block boundary in eastern China? (2001)
Faure, Michel, Lin, Wei, Le Breton, Nicole
The Qinling-Dabieshan belt results from the collision of the North China and South China blocks. The eastern extension of the belt (the Sulu area) consists of several stacked units: from top to...
Lin, Wei, Faure, Michel, Sun, Yan, Shu, Liangshu S., Wang, Qingchen
The Jiulingshan massif is an EW trending anticlinorium in the South China Block (SCB) that forms the southern foreland of the QinlingDabie orogen. The Jiulingshan consists of Middle Proterozoic...
Where is the North ChinaSouth China block boundary in eastern China? (2001)
Faure, Michel, Lin, Wei, Le Breton, Nicole
The Qinling-Dabieshan belt results from the collision of the North China and South China blocks. The eastern extension of the belt (the Sulu area) consists of several stacked units: from top to...
Wang, D.Z., Shu, Liangshu S., Faure, Michel, Zhan, Sheng
In SE China, a Mesozoic granitic dome coeval to extensional tectonics is exposed in the Wugongshan massif. Its center is occupied by Mesozoic granitoids and granitic gneisses, and the EW-trending...
Wang, D.Z., Shu, Liangshu S., Faure, Michel, Zhan, Sheng
In SE China, a Mesozoic granitic dome coeval to extensional tectonics is exposed in the Wugongshan massif. Its center is occupied by Mesozoic granitoids and granitic gneisses, and the EW-trending...
Lin, Wei, Faure, Michel, Sun, Yan, Shu, Liangshu S., Wang, Qingchen
The Jiulingshan massif is an EW trending anticlinorium in the South China Block (SCB) that forms the southern foreland of the QinlingDabie orogen. The Jiulingshan consists of Middle Proterozoic...
Where is the North ChinaSouth China block boundary in eastern China? (2001)
Faure, Michel, Lin, Wei, Le Breton, Nicole
The Qinling-Dabieshan belt results from the collision of the North China and South China blocks. The eastern extension of the belt (the Sulu area) consists of several stacked units: from top to...
Th. Etat : U.F.R. d'anglais, Etudes anglaises : Paris 10 Nanterre : 1995.
Thesis (doctoral)--Université de Paris X: Nanterre, 1995.
Thèse : Médecine : Lyon : 1978.
Vol. 2 : Planches et cartes hors-texte.
Les Collyres. Composition. Mise en forme. Contrôle. Aspects actuels. (1966)
Thèse. Pharm. Univ. Lyon. 1966. No 526.
Furge, Kyle A., Kiewlich, David, Le, Phuong, Vo, My Nga, Faure, Michel, Howlett, Anthony R., ...
Mutations in the Ras family of GTP binding proteins represent one of the most frequently observed genetic alterations in human cancers. We and others have recently demonstrated that expression of...
Furge, Kyle A., Kiewlich, David, Le, Phuong, Vo, My Nga, Faure, Michel, Howlett, Anthony R., ...
Mutations in the Ras family of GTP binding proteins represent one of the most frequently observed genetic alterations in human cancers. We and others have recently demonstrated that expression of...