Late Permian appinite–granite complex from northwestern Liaoning, North China Craton: Petrogenesis and tectonic implications
The appinite–granite suite commonly occurs within post-subduction regimes during the final stage of anorogeny and thus holds the key to monitoring critical geodynamic and crustal evolutionary processes. The present zircon U–Pb dating and geochemical study documents the Late Permian appinite–granite...
Main Authors: | , , , , |
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Format: | Journal Article |
Published: |
Elsevier BV
2012
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Subjects: | |
Online Access: | http://hdl.handle.net/20.500.11937/37812 |