Nd-O-Hf isotopic decoupling in S-type granites: Implications for ridge subduction
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DOI: 10.1016/j.lithos.2019.03.009
Abstract: Abstract The generation of S-type granites in the continental crust generally requires partial melting of metasedimentary rocks at relatively high temperatures, and is typically associated with syn- or post-collisional tectonics. These melts are generally expected… read more here.
Keywords: ridge subduction; type granites; melting metasedimentary; isotopic decoupling ... See more keywords