Dataset of PiaOac granites and deposits

Published: 23-02-2021| Version 1 | DOI: 10.17632/yxfssbmnk4.1
Jinhai Yu


This study presents zircon U-Pb ages and Hf isotope compositions and whole rock compositions of the PiaOac granites in NE Vietnam. These data indicate that the PiaOac granites were formed in Late Cretaceous and syn- to post-orogenic setting. The formation times of the granite and related mineralization are similar to those in SW South China. They consitute together a E-W trending Late Cretaceous magmatism and metallogeny belt. Their origin is related to the northward subduction of the Neo-Tethys Plate.


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