Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Yannis Bassias"'
Autor:
Claude Triboulet, Yannis Bassias
Publikováno v:
The Journal of Geology. 102:697-708
Metamorphism in the Taygetos (western Peloponnesus) and Parnon (eastern Peloponnesus) tectonic windows shows two distinct styles of evolution. The metamorphism in the Taygetos window shows at least two conventional clockwise P-T-t evolutionary paths
Autor:
Claude Triboulet, Yannis Bassias
Publikováno v:
Lithos. 28:1-19
Mineral and bulk rock chemistry of serpentinites recovered from the Southwest Indian Ridge (SWIR) at 62°E, east of the Melville Fracture Zone, are consistent with an origin as residual harzburgite products of low degrees of partial melting of a pare
Autor:
Yannis Bassias, Lucien Leclaire
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Monatshefte. 1990:67-90
Tectonothermal evolution of the late Panafrican Orogeny in the central Anti-Atlas (Southern Morocco)
Publikováno v:
The Atlas System of Morocco ISBN: 3540190864
Medium grade gneisses and metapelites from the northeastern Sirwa Mountains show complex retrograde pressure-temperature paths related to a lateral slip of a northern continental mass along the northern margin of the West African Craton. Early uplift
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27eaf38f09a6c28552a36cec6c06e6a8
https://doi.org/10.1007/bfb0011585
https://doi.org/10.1007/bfb0011585
Publikováno v:
Geochimica et Cosmochimica Acta. 53:2125-2131
The Kerguelen Plateau (South Indian Ocean), whose oldest age has been dated as early Cretaceous, shows geochemical and isotopic features characteristic of OIB-type magmatism. It is probably related to the early stages of activity of the Kerguelen hot
Autor:
Micheline Denis-Clocchiatti, Bernard Gensous, Hugh L Davies, Pierre-Jean Giannesini, Lucien Leclaire, Jacques Segoufin, Yannis Bassias, Philippe Patriat, Michel Tesson, Isabelle Gautier, Jacques Wannesson
Publikováno v:
Geo-Marine Letters. 7:169-176
Geological samples from the southern Kerguelen Plateau include Lower Cretaceous basalt and lava breccia, probable Lower Cretaceous conglomerate and shelf limestone, Upper Cretaceous chert with dolomite, Upper Cretaceous-Eocene ooze, and Tertiary cong