The overall stratigraphic thickness of the Xishanyao Formation shows a decreasing trend near the Xidagou Syncline and the axis of the Huoshaoshan Anticline, indicating that the anticline had already developed prior to coal seam deposition and subsequently experienced uplift.
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Late Cenozoic exhumation in the eastern Junggar Basin: Evidence from zircon (U-Th)/He ages of combustion metamorphic rocks.
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