Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Michel Delaloye"'
Autor:
Ömer Faruk Çelik, Michel Delaloye
Publikováno v:
Journal of Asian Earth Sciences. 26:461-476
Small outcrops of the metamorphic rocks of the Beysehir ophiolite appear to the west of Gencek and to the south of Durak (South of Beysehir Lake) in the Central Tauride Belt in Turkey. Amphibolitic rocks in the ophiolitic melange have an igneous orig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f5bdba748af337363a5ed1179df46c8
https://doi.org/10.1016/j.jseaes.2004.10.008
https://doi.org/10.1016/j.jseaes.2004.10.008
Publikováno v:
Geological Magazine. 143:213-227
The Tauride Belt Ophiolites in southern Turkey are located on both sides of the E–W-trending, Mesozoic Tauride carbonate platform. They comprise the Lycian, Antalya, Beyşehir, Mersin, Alihoca and Pozantı-Karsantı ophiolites from west to east. Ea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6031957ffa24c126beb900497859610
https://doi.org/10.1017/s0016756805001524
https://doi.org/10.1017/s0016756805001524
Granitoids from Western and Northwestern Anatolia: Geochemistry and Modeling of Geodynamic Evolution
Autor:
Erguzer BlNGOL, Michel Delaloye
Publikováno v:
International Geology Review. 42:241-268
Magmatic rocks of variable age and composition crop out extensively in Western and Northwestern Anatolia. In the present study we subdivide these granitoids according to their ages. The young granitoids (Late Cretaceous to Late Miocene) develop high-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b5adb793289818d1dcbdcc376603366
https://doi.org/10.1080/00206810009465081
https://doi.org/10.1080/00206810009465081
Autor:
Osman Parlak, Michel Delaloye
Publikováno v:
Tectonophysics. 301:145-158
The Mersin ophiolite is located on the southern flank of the E-W-trending central Tauride belt in Turkey. It is one of the Late Cretaceous Neotethyan oceanic lithospheric remnants. The Mersin ophiolite formed in a suprasubduction zone tectonic settin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::66ad21b6562ea47eb72ee0be1deaf527
https://doi.org/10.1016/s0040-1951(98)00222-4
https://doi.org/10.1016/s0040-1951(98)00222-4
Publikováno v:
Journal of African Earth Sciences. 24:259-269
Resume Les regions du Rekkame, du Moyen Atlas et du Maroc Central presentent de nombreux centres volcaniques d'aˆge Paleogene, Neogene et Quaternaire. Dans la majoritedes cas, il s'agit d'epanchements de basanites et de nephelinites. Dans la provinc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::436f38aba941661d31ad4a08e1e1a67d
https://doi.org/10.1016/s0899-5362(97)00042-0
https://doi.org/10.1016/s0899-5362(97)00042-0
Autor:
Osman Parlak, Michel Delaloye
Publikováno v:
Terra Nova. 8:585-592
WOS: A1996WG68700011 The Mersin ophiolite, which is a relic of the late Cretaceous Neotethyan ocean domain in the eastern Mediterranean, is situated on the southern flank of the central Tauride belt. The ophiolite body is cross-cut at all structural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e36d79a019eafc1ab39dcaa09a47e1ec
https://doi.org/10.1111/j.1365-3121.1996.tb00788.x
https://doi.org/10.1111/j.1365-3121.1996.tb00788.x
Publikováno v:
International Geology Review. 38:778-786
The Mersin ophiolite is an ~6-km-thick oceanic crustal sequence in the central Taurides (southern Turkey), forming large outcrops on the southern flank of Bolkardag. It comprises a sequence of units and includes, in ascending structural order, the Me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d1ea8958786f78facc41dacced43889f
https://doi.org/10.1080/00206819709465361
https://doi.org/10.1080/00206819709465361
Publikováno v:
Journal of African Earth Sciences, Vol. 17, No 3 (1993) pp. 333-341
Le Jbel Saghro est un des deux grands appareils volcaniques alcalins récents de l'Anti-Atlas. Les laves émises sont des néphélinites à olivine, des téphrites et des phonolites. Les phonolites suivent un chemin de différentiation particulier, s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::941d44cf7eda88b66dcb02d44c8b74fb
https://doi.org/10.1016/0899-5362(93)90077-4
https://doi.org/10.1016/0899-5362(93)90077-4
A number of Late Cretaceous ophiolitic bodies are located between the metamorphic massifs of the southeast Anatolian orogenic system. One of them, the Göksun ophiolite (northern Kahramanmaraş), which crops out in a tectonic window bounded by the Ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2697b9e87d92248a248275ef99ad5edc
https://hdl.handle.net/20.500.12605/18090
https://hdl.handle.net/20.500.12605/18090
Autor:
Michel Delaloye, Ö. Faruk Çeli̇k
Publikováno v:
Geological Journal, Vol. 38, No 3-4 (2003) pp. 235-256
The Antalya and Lycian ophiolites are situated in the western part of the Tauride belt (SW Turkey). Ophiolite-related metamorphic sole rocks in the Tauride belt are observed either at the base of the tectonites or in melange units. Geochemical observ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c931a1e8a0c8645d086fafe8dcdab6c4
https://archive-ouverte.unige.ch/unige:151472
https://archive-ouverte.unige.ch/unige:151472