Detrital zircon U-Pb ages of the Proterozoic metaclastic-sedimentary rocks in Hainan Province of South China: New constraints on the depositional time, source area, and tectonic setting of the Shilu Fe-Co-Cu ore district
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文摘

Shihuiding Formation is re-interpreted as the top, Seventh member of the Shilu Group.

Shilu Group and interbedded BIFs have a maximum depositional time of 1070–970 Ma.

A marine, retroarc foreland basin proposed for the host rocks and interbedded BIFs.

Precursors to the Shilu Group were dominantly derived from Laurentia.

Hainan Island was most likely attached or close to northwestern Laurentia in Rodinia.

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