Zobrazeno 1 - 10
of 81
pro vyhledávání: '"R. Montigny"'
Publikováno v:
Tectonophysics. 296:103-123
Spinel peridotite bodies from the North Pyrenean Zone (NPZ) contain ubiquitous anhydrous pyroxenite layers and, in the Lherz area exclusively, late dykes or veins of amphibole pyroxenites and hornblendites cross-cutting the layering. Anhydrous and am
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::727badf7baba32263767f961bf0cc29b
https://doi.org/10.1016/s0040-1951(98)00139-5
https://doi.org/10.1016/s0040-1951(98)00139-5
Publikováno v:
Journal of South American Earth Sciences. 7:149-165
The Campo Formoso and Carnaiba granites belong to a suite of middle Proterozoic magmatic rocks located in the northern part of the Sao Francisco craton. They intrude the Archaen basement and Lower Proterozoic Jacobina volcanosedimentary series. Emera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b455940db1e4acba4f14f7985549c0f5
https://doi.org/10.1016/0895-9811(94)90005-1
https://doi.org/10.1016/0895-9811(94)90005-1
Autor:
Rainer Thomas, Patrik Konečný, J. Kráľ, Karel Schulmann, Walter Prochaska, Ondrej Lexa, W. Frank, R. Montigny, Vratislav Hurai, Martin Chovan
Publikováno v:
Geofluids
Geofluids, Wiley, 2008, 8 (3), pp.181-207. ⟨10.1111/j.1468-8123.2008.00216.x⟩
Geofluids, Wiley, 2008, 8 (3), pp.181-207. ⟨10.1111/j.1468-8123.2008.00216.x⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1915e9b20caf0e1f1b375440c5c745d3
https://hal.archives-ouvertes.fr/halsde-00364034
https://hal.archives-ouvertes.fr/halsde-00364034
Publikováno v:
Canadian Journal of Earth Sciences. 16:2150-2164
Paleomagnetism and K–Ar dating of Permian, Triassic, and Cretaceous rocks from Morocco. We have sampled and studied volcanic rocks from the whole of Morocco. Permo-Carboniferous rocks give a magnetic pole situated at 36°N and 238°E (four sites, K
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e681d377c8a2bcb2f8bbd9e2de1efa54
https://doi.org/10.1139/e79-202
https://doi.org/10.1139/e79-202
Publikováno v:
Geological Society, London, Special Publications. 13:121-130
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9490641fc23e1d295a3e81ac733880ec
https://doi.org/10.1144/gsl.sp.1984.013.01.11
https://doi.org/10.1144/gsl.sp.1984.013.01.11
Publikováno v:
Journal of Geophysical Research: Solid Earth. 89:3315-3333
A recent model proposes that Afar is one of the few areas in the world where the formation of a passive margin by rift propagation can be observed directly. Forty sites spread over approximately 10,000 km2 in the Republic of Djibouti, between the Asa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::457d80e3b232c75dc40efc1ee1343048
https://doi.org/10.1029/jb089ib05p03315
https://doi.org/10.1029/jb089ib05p03315
Autor:
M. Misseri, R. Montigny, Françoise Boudier, Jean-Luc Bouchez, Georges Ceuleneer, Mathilde Cannat, Adolphe Nicolas
Publikováno v:
Earth and Planetary Science Letters. 75:215-222
Kinematics of early thrusting of Oman ophiolites is deduced using analysis of homogeneous deformation in their metamorphic soles, and is constrained by new K Ar ages. A model of decollement from a Tethyan ridge system is proposed for the 100-95 Ma pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d65306dd8f918ea43f85da7770766fc
https://doi.org/10.1016/0012-821x(85)90103-7
https://doi.org/10.1016/0012-821x(85)90103-7
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 168:358-388
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::372593e98bc4fe977a4f9a4cf6883819
https://doi.org/10.1127/njgpa/168/1984/358
https://doi.org/10.1127/njgpa/168/1984/358
Publikováno v:
Tectonophysics. 129:257-273
K-Ar measurements on minerals extracted from alkaline magmatic rocks evenly distributed along the Pyrenean belt show that magmatic activity took place between 110 and 85 Ma. Three age groups are observed: the first falls around 110 Ma, the second and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91c035033f08d60c89d725339f1c7be2
https://doi.org/10.1016/0040-1951(86)90255-6
https://doi.org/10.1016/0040-1951(86)90255-6
Publikováno v:
Geochimica et Cosmochimica Acta. 37:2135-2147
Abundances of major elements, rare earth elements, transition metals, alkali metals and alkaline earth metals have been measured in a representative suite of samples from the Pindos (Greece) ophiolitic complex. Our data indicate that the igneous memb
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2fa945233e9b74292d179d3c3458d609
https://doi.org/10.1016/0016-7037(73)90012-4
https://doi.org/10.1016/0016-7037(73)90012-4