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U-Pb age and Hf-O isotopes of detrital zircons from Hainan Island: Implications for Mesozoic subduction models
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文摘

Identification of a sharp ca. 120 Ma age peak in detrital zircons of Hainan Island.

Decode sedimentary provenances, regional magmatic barcode and tectonic evolution.

The Hf-O isotopic compositions suggest progressive crustal growth during the Mesozoic.

Mesozoic magmatism in SE China was part of the circum-Pacific accretionary orogens.

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