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pro vyhledávání: '"Leonardo A. Agulleiro Insúa"'
Autor:
Jasper Berndt, Manuel Demartis, Stefan Jung, Leonardo A. Agulleiro Insúa, Lucio Pedro Pinotti, Jorge E. Coniglio, Ana María Sato, María Natalia Maffini, Fernando Javier D'eramo, Stefania Radice, Eugenio Aragón
The Comechingones pegmatitic field comprises granitic pegmatites and leucogranites hosted by mylonitic rocks from the Guacha Corral shear zone. Pegmatites consist of variably sized, internally zoned bodies, with late replacement units. Leucogranites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de9446ad7cd8c915c7e8c45bc1bd4cea
http://linkinghub.elsevier.com/retrieve/pii/S0895981117300883
http://linkinghub.elsevier.com/retrieve/pii/S0895981117300883
Autor:
José María Tubía, Leonardo A. Agulleiro Insúa, Lucio Pedro Pinotti, Manuel Demartis, Jorge E. Coniglio, Eugenio Aragón, Fernando Javier D'eramo
Publikováno v:
Journal of Structural Geology. 33:1334-1346
Ordovician to Devonian aged crustal-scale Guacha Corral shear zone (GCSZ), central Argentina, hosts rare element pegmatites of the Comechingones pegmatitic field (CPF). In the CPF an eastwards decreasing strain gradient related to the GCSZ deformatio