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The provenance of the middle Miocene deep-water sedimentary rocks was studied by detrital zircon U-Pb ages and heavy mineral assemblages in the Yinggehai-Song Hong Basin. U-Pb age data for 936 detrital zircons from eleven sedimentary rock samples from the Meishan Formation (Langhian-Serravallian) range in age from 3252 Ma to 28 Ma and suggests input from multiple sources. The provenance of the sediments...
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