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pro vyhledávání: '"W. F. Hoover"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 8, Pp n/a-n/a (2023)
Abstract Talc‐rich rocks are common in exhumed subduction zone terranes and may explain geophysical observations of the subduction zone interface, particularly beneath Guerrero, Mexico, where the Cocos plate subducts horizontally beneath North Amer
Externí odkaz:
https://doaj.org/article/4052af618e2945b6b9cbb707113fe075