Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Clara E. Cisterna"'
Autor:
Silvana Elizabeth Marangone, Anja M. Schleicher, Kathleen Marie Griffin, Uwe Altenberger, Fernando Guillermo Sardi, Clara E. Cisterna
Publikováno v:
Journal of South American Earth Sciences
The Villismán pegmatite group belonging to the Ancasti district of the Pampean Pegmatite Province is geologically formed by banded schists of the Ancasti Formation which are intruded by the homonymous granitic stock and Li-pegmatites. It is located
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f29c4165d2f5e702a001b95b0a789caa
https://doi.org/10.1016/j.jsames.2020.102764
https://doi.org/10.1016/j.jsames.2020.102764
Autor:
Beatriz Lidia Luisa Coira, Clara E. Cisterna, Magdalena Maria L. Koukharsky, S. Rivero Guevara
Publikováno v:
Journal of South American Earth Sciences. 27:24-35
Geochemical characteristics of Ordovician basic volcanic rocks help to define the evolving tectonic setting of the Argentine Puna and northern Chile. Four spatially distinct magmatic groups are defined on geological, petrographical, geochemical and i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee59e43e85a5d50215bfff3b0f5a7a95
https://doi.org/10.1016/j.jsames.2008.10.002
https://doi.org/10.1016/j.jsames.2008.10.002
Autor:
Clara E. Cisterna
Publikováno v:
Estudios Geológicos. 48
The granitoids from the Sierra de Narvaez were investigated for their geochemical and petrographical characteristics. They are composed of calc-alkaline granites, granodiorites and tonalites, similar to the other paleozoic granitoids of the Famatina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9b428fb420d209e6a5160aca04f2f920
https://doi.org/10.3989/egeol.92485-6389
https://doi.org/10.3989/egeol.92485-6389