Slab window-related magmatism from southernmost South America: the Late Miocene mafic volcanics from the Estancia Glencross Area (ca. 52°S, Argentina?Chile)

Autor: D'Orazio M. 1), Agostini S. 3), Innocenti F. 1), Haller M.J. 2), Manetti P. 3), Mazzarini F. 3)

Publikováno v: Lithos (Oslo. Print) 57 (2001): 67–89.
info:cnr-pdr/source/autori:D'Orazio M. 1), Agostini S. 3), Innocenti F. 1), Haller M.J. 2), Manetti P. 3), Mazzarini F. 3)/titolo:Slab window-related magmatism from southernmost South America: the Late Miocene mafic volcanics from the Estancia Glencross Area (ca. 52°S, Argentina?Chile)/doi:/rivista:Lithos (Oslo. Print)/anno:2001/pagina_da:67/pagina_a:89/intervallo_pagine:67–89/volume:57

The Estancia Glencross Area EGA volcanic rocks form a series of five isolated buttes located at the southern end ca. 52°S of the discontinuous belt of Cenozoic basaltic lava formations occurring in the extra-Andean Patagonia. EGA volcanics are subal

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http://www.cnr.it/prodotto/i/29050