Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Jean-Claude Guezou"'
Publikováno v:
Geological Journal. 57:1125-1136
Publikováno v:
Journal of Neutron Research. 9:357-362
The residual elastic strains determination by neutron diffraction has been performed on quartzite samples from a former texture study. The measured complete residual strain tensor has been considered as representative of the “natural” finite plas
Autor:
Thierry Baudin, Marie-Hélène Mathon, Monica Ceretti, Richard Penelle, Jean-Michel Sprauel, Jean-Claude Guezou
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 328:733-738
Residual elastic strain determination by neutron diffraction has been performed on quartzite samples from an earlier texture study. The main objective of this study is to derive a complete strain tensor of a natural deformation for a later introducti
Publikováno v:
Journal of Structural Geology. 17:233-244
Folds with axes almost parallel to the mean tectonic transport direction are frequent in fold-thrust belts, particularly along the borders of arcuate belts. Such structures have been frequently explained in terms of superimposed tectonic events but,
Publikováno v:
Geological Journal. 28:239-250
Workshop on the Geology of Turkey -- APR, 1992 -- KEELE UNIV, KEELE, ENGLAND
WOS: A1993MU79900003
The eastern end of the Sivas Basin, just west of Erzincan, is known as the Kemah Basin. The lithostratigraphy of the Kemah Basin thus correspo
WOS: A1993MU79900003
The eastern end of the Sivas Basin, just west of Erzincan, is known as the Kemah Basin. The lithostratigraphy of the Kemah Basin thus correspo
Publikováno v:
Bulletin de la Société Géologique de France. 162:611-626
Publikováno v:
Tectonics. 24
[1] We present the first complete balanced cross section across the southeastern Zagros fold-thrust belt (ZFTB). The following main structural features emerge from this section: (1) In the south of the ZFTB, the Proterozoic-to-Recent sedimentary sequ
Publikováno v:
Tectonophysics
Tectonophysics, 2005, 411, pp.89-109
Tectonophysics, Elsevier, 2005, 411, pp.89-109
Tectonophysics, 2005, 411, pp.89-109
Tectonophysics, Elsevier, 2005, 411, pp.89-109
The Zagros Simple Fold Belt is characterized by elongated, curved, or sigmoidal folds. The trend of these structures together with the structural style, change suddenly across the Zagros–Makran syntaxis which separates the continental collision dom
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::68908a9595c50e37b44a3b14c2f09bff
https://hal.science/hal-00143652
https://hal.science/hal-00143652
Publikováno v:
Marine and Petroleum Geology
Marine and Petroleum Geology, 2004, 21, pp.735-752
Marine and Petroleum Geology, Elsevier, 2004, 21, pp.735-752
Marine and Petroleum Geology, 2004, 21, pp.735-752
Marine and Petroleum Geology, Elsevier, 2004, 21, pp.735-752
The Bandar Abbas syntaxis marks the transition between the Zagros collisional belt and the Makran subduction-related prism and constitutes a major structural feature within the Alpine–Himalayan mountain belt. Within the foreland part of the Zagros
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1536ae3b1d2abae6658bdfebdbf9a5bf
https://hal.science/hal-00067776
https://hal.science/hal-00067776
Publikováno v:
Bulletin de la Société Géologique de France
Bulletin de la Société Géologique de France, 2003, 174 (2), pp.107-114
Bulletin de la Société Géologique de France, Société géologique de France, 2003, 174 (2), pp.107-114
Bulletin de la Société Géologique de France, 2003, 174 (2), pp.107-114
Bulletin de la Société Géologique de France, Société géologique de France, 2003, 174 (2), pp.107-114
The emplacement of the Saint-Brieuc diorite (533 ± 12 Ma ; Brittany, France) developed a narrow contact aureole in metabasaltic host-rocks which were previously submitted to a regional-scale deformation and metamorphism at around 590-570 Ma. This st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f625b3d57d7857ed9154efcac52c8927
https://hal.science/hal-00069154
https://hal.science/hal-00069154