Ultra-high temperature metamorphism in the Guaxupé Complex: a lower crust segment
نویسندگان
چکیده
منابع مشابه
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In some places, there is strong evidence that the lower continental crust has flowed so as to smooth out variations in crustal thickness caused by differential crustal extension or shortening. In order to better understand the processes involved, we investigate the behavior of a fluid layer over a fluid half-space to see how such a system responds to the deformation of its upper and lower bound...
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ژورنال
عنوان ژورنال: Brazilian Journal of Geology
سال: 2020
ISSN: 2317-4692,2317-4889
DOI: 10.1590/2317-4889202020200005