Article ID Journal Published Year Pages File Type
5784140 Lithos 2017 51 Pages PDF
Abstract
Both the upper and lower layers of the Heiyingshan garnet-bearing rhyolites show typical S-type affinity, such as the radioactive 87Sr/86Sr and low ε(Nd) and ε(Hf) values indicating they were derived from the partial melting of the metasedimentary rocks. These characteristics are clearly distinct from those of the Permian A-type granitoids, providing new evidence for the crustal reworking in the CAOB.215
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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