Zobrazeno 1 - 10
of 49
pro vyhledávání: '"Philippe Matte"'
Autor:
Jean-Marc Lardeaux
Publikováno v:
Comptes Rendus Geoscience. 341:95-96
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7389f790f229265bea6d020243db73e1
https://doi.org/10.1016/j.crte.2009.01.004
https://doi.org/10.1016/j.crte.2009.01.004
Akademický článek
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Autor:
Philippe Matte
Publikováno v:
Geological Society, London, Memoirs. 32:421-426
The Urals are a linear north-south-trending belt (2500 km in length, from Novaya Zemlya to the Aral Sea). Their apparent narrowness (100-150 km) in the polar and cispolar parts is mainly due to the Siberian Meso-Cenozoic post-tectonic cover. In the s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07af6e1436c496c0c11b589f4ab39f40
https://doi.org/10.1144/gsl.mem.2006.032.01.25
https://doi.org/10.1144/gsl.mem.2006.032.01.25
Publikováno v:
Comptes Rendus Geoscience. 336:19-28
Resume Dans la zone axiale de la Montagne noire (Massif central francais), nous avons date pour la premiere fois par la methode U–Pb sur zircons, les orthogneiss œilles d'affinite calco-alcaline qui constituent le cœur du dome gneissique. Deux ec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4644f09d8620620fb16edd114a5f3545
https://doi.org/10.1016/j.crte.2003.10.014
https://doi.org/10.1016/j.crte.2003.10.014
Autor:
Philippe Matte
Publikováno v:
Comptes Rendus Geoscience. 334:773-779
The Palaeozoic of the western Pyrenees shows two superposed tectonics easily defined by their different geometry and the major unconformity of the Permian sediments and volcanics on the Devono-Carboniferous series: an Hercynian tectonic found only in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcaceb245539854c7302e634c129ab68
https://doi.org/10.1016/s1631-0713(02)01808-4
https://doi.org/10.1016/s1631-0713(02)01808-4
Autor:
Philippe Matte
Publikováno v:
GFF. 120:209-222
Most of the Phanerozoic orogenic belts exhibit HP to UHP metamorphism. First discovered in the Alps and the Norwegian Caledonides, ultra-high pressure rocks are now described in various Paleozoic belts including the Kazakhstan Caledonides, the Uralid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf6e0218c3a65ddc7de7d438068c1dd4
https://doi.org/10.1080/11035899801202209
https://doi.org/10.1080/11035899801202209
Publikováno v:
Geodinamica Acta. 11:13-22
Resume Recemment, on a tente d'expliquer lu formation des domes gneissiques de la chaine hercynienne et notamment celui de la Montagne Noire (Sud du Massif Central francais), par un modele purement extensif de type “Basin and Range”. D'apres ce m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::220a997683061478173a8dbfdec39124
https://doi.org/10.1080/09853111.1998.11105308
https://doi.org/10.1080/09853111.1998.11105308
Autor:
Maurice Mattauer, Philippe Matte
Publikováno v:
Geodinamica Acta. 11:23-31
Resume La region de St-Etienne (bassin houiller el massif metamorphique du Mt Pilat) est une de celles ou l'on a formule pour la premiere fois dans le Massif Central francais la notion de “late orogenic extension” pour la chaine hercynienne. L'ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42a98bdf5385bd01da665b711acc82ba
https://doi.org/10.1016/s0985-3111(98)80026-0
https://doi.org/10.1016/s0985-3111(98)80026-0
Publikováno v:
Tectonophysics. 276:217-227
A new evolutionary geodynamic model of Devonian continental subduction and exhumation of high-pressure/low-temperature metamorphic rocks in the southern Urals is proposed based on the results of physical modelling, geological and geophysical data, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5aa7d807eff5050a86179caa750c1ecb
https://doi.org/10.1016/s0040-1951(97)00057-7
https://doi.org/10.1016/s0040-1951(97)00057-7
Publikováno v:
Tectonophysics. 223:313-337
The 40Ar-39Ar dating method has been applied to mylonitic rocks from the Carpathian mountains. These are Variscan metamorphic and magmatic rocks that were overprinted during the Alpine orogeny. The Inner Western Carpathians are conventionally describ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6baf95e915024d14752f49dd0a015060
https://doi.org/10.1016/0040-1951(93)90143-8
https://doi.org/10.1016/0040-1951(93)90143-8