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Provenance and sediment dispersal of the Triassic Yanchang Formation, southwest Ordos Basin, China, and its implications
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The Yanchang Formation in the southern Ordos Basin was locally sourced from basin marginal deformation belts

Lower and middle sections were derived from the north Qinling Orogenic belt and recycled Proterozoic to Paleozoic sedimentary rocks

The lower and middle sections were mainly derived from the north Qinling Orogenic belt and recycled Proterozoic to Paleozoic sedimentary rocks;

Upper section was sourced from the Qilian-Qaidam terranes and west Qinling Orogenic belt

The Liupanshan thrust and fold belt became an active source starting at the upper section of the Yanchang Formation

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