Article ID Journal Published Year Pages File Type
4716652 Lithos 2012 21 Pages PDF
Abstract
► Zircon U-Pb age indicates that the deposition of the Haizhou Group was later than ~610 Ma. ► In situ Hf isotopic data indicates these rocks were derived from reworking of Paleoproterozoic to Archean crust. ► The results support the suture between the NCB and SCB is the B-Y Fault.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Zircon U-Pb and Lu-Hf isotope study of the Neoproterozoic Haizhou Group in the Sulu orogen: Provenance and tectonic implications
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