Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Magmatismo básico"'
Publikováno v:
Geologia USP. Série Científica, Vol 18, Iss 2 (2018)
Intrusões dioríticas, gabroicas e outras rochas máficas-ultramáficas registram tanto os processos de extração e transporte de magmas do manto, resultando na acresção vertical de material à crosta, quanto os processos de interação entre ess
Externí odkaz:
https://doaj.org/article/a4440a11ca72470587041299dc2d583c
Publikováno v:
Anais da Academia Brasileira de Ciências, Vol 75, Iss 3, Pp 331-339 (2003)
The Arenópolis volcano-sedimentary sequence is located in the southern part of the Goiás Magmatic Arc and includes a ca. 900 Ma calc-alkaline arc sequence made of volcanic rocks ranging in composition from basalts to rhyolites, metamorphosed under
Externí odkaz:
https://doaj.org/article/eeaecf188c5e4e4db48ef41dbef9d1e0
Publikováno v:
Estudios Geologicos, Vol 54, Iss 5-6, Pp 191-197 (1998)
Rocas volcánicas submarinas (lavas almohadilladas) aparecen intercaladas entre calizas margosas y margas de la Formación Capas Rojas del Subbético Medio. La datación con nannoplancton de los materiales inmediatamente infrayacentes y suprayacentes
Externí odkaz:
https://doaj.org/article/10c66709baf9498c9ca259aab9db0deb
Publikováno v:
Estudios Geologicos, Vol 51, Iss 3-4, Pp 109-118 (1995)
El magmatismo básico mesozoico de las Zonas Externas de las Cordilleras Béticas (ZECB) está representado por bloques tectónicos de pequeñas dimensiones («ofitas») intercalados entre los sedimentos arcilloso-yesíferos del Trías Keuper y por n
Externí odkaz:
https://doaj.org/article/002a486f6fc84f9d8f0e51e4d6321211
Publikováno v:
Geologia USP. Série Científica, Vol 18, Iss 2 (2018)
Intrusões dioríticas, gabroicas e outras rochas máficas-ultramáficas registram tanto os processos de extração e transporte de magmas do manto, resultando na acresção vertical de material à crosta, quanto os processos de interação entre ess
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d6c2872d13c17d6e805a2b12e58d8a1b
https://doi.org/10.11606/issn.2316-9095.v18-125442
https://doi.org/10.11606/issn.2316-9095.v18-125442
Publikováno v:
Estudios Geologicos, Vol 54, Iss 5-6, Pp 191-197 (1998)
Submarine volcanic rocks (pillow lavas) appear into the marly limestones and marls of the Capas Rojas Formation in the Median Subbetic. The dating with nannoplankton of the immediately underlying and overlying materials to these volcanic rocks has al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doajarticles::a162468efd481d4cc93d404602089179
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/218/219
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/218/219
Publikováno v:
Estudios Geologicos, Vol 51, Iss 3-4, Pp 109-118 (1995)
The Mesozoic basic magmatism found in the External Zones of the Betic Cordilleras (ZECB) is represented either as «ophites» forming small dimension tectonic blocks intercalated in the Keuper gypsum-rich, clay sediments, or also as lava ilow bod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doajarticles::c384b6bec026a0b5c3a2fddddcdc20f3
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/289/292
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/289/292
Autor:
Navarrete Rodriguéz, Angela Teresa, Moreno-Murillo, Juan Manuel, Concha Perdomo, Ana Elena, Patarroyo Gama, Pedro
Publikováno v:
Repositorio UN
Universidad Nacional de Colombia
instacron:Universidad Nacional de Colombia
Universidad Nacional de Colombia
instacron:Universidad Nacional de Colombia
Close to the Pacho town it is exposed a basic intrusive body of conic morphology, named as Gabbro Tragarepas intruding sedimentary rocks of Albian age. Petrographically intrusive rocks are composed of plagioclase labradorite, augite and hornblende, c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::50056eae27a1e18e7dc91319f49ac19f
https://repositorio.unal.edu.co/handle/unal/42109
https://repositorio.unal.edu.co/handle/unal/42109
