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Soft‐sediment deformation structures are abundant in the upper part of the Upper Triassic Tanzhuang Formation in the Jiyuan district, southern North China Craton. These deformation structures include large load casts, flame structures, ball‐and‐pillow structures, lenticular sand bodies, synsedimentary faults, and slump structures. The lenticular sand bodies, synsedimentary faults, and slump structures...
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