Sedimentological and geochronological constraints on the Carboniferous evolution of central Inner Mongolia, southeastern Central Asian Orogenic Belt: Inland sea deposition in a post-orogenic setting
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Five sedimentary stages were distinguished from the Carboniferous strata.

Detrital zircon dating revealed that the provenances were mainly local magmatic rocks.

Upper Carboniferous strata were deposited in an inland sea after an orogenic event.

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