Zobrazeno 1 - 10
of 48
pro vyhledávání: '"zoned pluton"'
Publikováno v:
Journal of Maps, Vol 13, Iss 2, Pp 684-697 (2017)
The Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence
Externí odkaz:
https://doaj.org/article/6d8a1bce34dc42749a865fce9205196d
Publikováno v:
研究紀要. 57:41-69
The Okueyama Granitic Complex exhibits vertical compositional zonation. The whole-rock SiO2 content increases from 66 to 73wt.％ as the altitude increases from about 300m at the bottom to 1,300m at the roof. The TiO2, Al2O3, FeO＊, MgO, CaO, Na2O,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::95dca3563ba2548bd92d06650585fe36
https://repository.nihon-u.ac.jp/xmlui/handle/11263/2283
https://repository.nihon-u.ac.jp/xmlui/handle/11263/2283
Publikováno v:
Centro de Investigación Científica y de Educación Superior de Ensenada
CICESE
Repositorio Institucional CICESE
CICESE
Repositorio Institucional CICESE
El plutón zonado La Primavera forma parte de un complejo batolítico que aflora en un área de más de 500 km2 al sur del Cinturón Batolítico Peninsular del Cretácico (29°N y 114°W). Dicho cuerpo es un stock que se caracteriza por presentar una
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3056::c3532800c46e4e7b1a6312be98986492
http://cicese.repositorioinstitucional.mx/jspui/handle/1007/3537
http://cicese.repositorioinstitucional.mx/jspui/handle/1007/3537
Akademický článek
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Publikováno v:
Journal of Maps, Vol 13, Iss 2, Pp 684-697 (2017)
The Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5556a853834dde8a2409824416a24468
Akademický článek
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Autor:
Omar Gianola, Max W. Schmidt, Eric Reusser, Irena Peytcheva, Albrecht von Quadt, Pietro Luraschi
Publikováno v:
Swiss Journal of Geosciences, 107 (2-3)
The calc-alkaline Bergell intrusion is classically mapped as a main tonalite and main granodiorite unit, whose ages have been determined at 32 and 30 Ma, respectively. These units are separated by a mostly thin band interpreted as magmatic “transit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5833584a386bf07090dfa97c54cbda4a
https://hdl.handle.net/20.500.11850/94779
https://hdl.handle.net/20.500.11850/94779
Publikováno v:
Proceedings of the NIPR Symposium on Antarctic Geosciences. 9:76-90
The subvolcanic granitic pluton in the Barton and Weaver Peninsulas, King George Island, is mainly composed of granodiorite with small volumes of gabbro, diorite and aplitic dikes. The pluton shows a vertically compositional zonation; the lower part
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::58e49126a6004efd1e489d7848966562
http://id.nii.ac.jp/1291/00002825/
http://id.nii.ac.jp/1291/00002825/
Akademický článek
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Autor:
Isabel Margarida Horta Ribeiro Antunes, Ana Margarida R. Neiva, Maria Manuela Silva, Fernando Corfu
Publikováno v:
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
The zoned pluton from Castelo Branco consists of Variscan peraluminous S-type granitic rocks. A muscovite>biotite granite in the pluton's core is surrounded successively by biotite>muscovite granodiorite, porphyritic biotite>muscovite granodiorite gr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c13c3937ad7c1900a9cd9647397d511c
https://hdl.handle.net/10316/3925
https://hdl.handle.net/10316/3925