Zobrazeno 1 - 6
of 6
pro vyhledávání: '"J. D. de la Rosa"'
Publikováno v:
Estudios Geologicos, Vol 66, Iss 2, Pp 157-169 (2010)
El plutón San Cristóbal constituye un cuerpo granítico de 35 km2 que aflora en el extremo sudeste de la Sierra de Velasco, situada al oeste de la ciudad de La Rioja, Argentina. Está formado por monzogranitos y sienogranitos con escasas granodiori
Externí odkaz:
https://doaj.org/article/4dba60477f394703878603096426ceff
Autor:
M, In 't Veld, C, Carnerero, J, Massagué, A, Alastuey, J D, de la Rosa, A M, Sánchez de la Campa, M, Escudero, E, Mantilla, G, Gangoiti, C Pérez, García-Pando, M, Olid, J R, Moreta, J L, Hernández, J, Santamaría, M, Millán, X, Querol
Publikováno v:
The Science of the total environment. 777
The Guadalquivir Valley is one of three major O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::f2bf7a038575e1e426a3e523cf6d8edd
https://pubmed.ncbi.nlm.nih.gov/33677295
https://pubmed.ncbi.nlm.nih.gov/33677295
Publikováno v:
Earth-Science Reviews. 31:237-253
Recent studies on calc-alkaline plutonic rocks reveal field and petrographic relationships with strong implications for the processes involved in their genesis. The presence of magmatic inclusions and magma mingling zones in these rocks supports an o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d03cfad7a5c5d47a8ea186c04ca7aec
https://doi.org/10.1016/0012-8252(91)90020-g
https://doi.org/10.1016/0012-8252(91)90020-g
Publikováno v:
Geologische Rundschau. 80:109-120
The crystallization sequence, nucleation density and crystal index (n = nucleation density/mode) of tonalitic enclaves from different granitoids of the Hercynian orogeny indicate that they are pieces of magma partially crystallized in the interior of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a59f79ab69de6377daf36faf695f290e
https://doi.org/10.1007/bf01828770
https://doi.org/10.1007/bf01828770
Publikováno v:
Geological Journal. 25:391-404
Many Hercynian granitoids of calc-alkaline composition are characterized by the presence of microgranular enclaves of tonalite to diorite composition. Though some differences in size, shape, and relative abundance of the enclaves are observed between
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3e7cb294e65c11246f991ceecde2eff
https://doi.org/10.1002/gj.3350250321
https://doi.org/10.1002/gj.3350250321
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