Inversion method of microscale deposition stage palaeogeomorphology in weak construction deformation range
A deformation zone and small-scale technology, applied in the field of geological and mineral exploration, can solve problems that affect sedimentation and reservoir research work, stay, and cannot fully reflect paleogeomorphology
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[0048] The Ordos Basin is divided into six first-level structural units, including the western margin thrust belt, Tianhuan depression, Yimeng uplift, Yishan slope, western Shanxi perturbation belt and Weibei uplift. The western marginal thrust belt and the western Shanxi disturbance zone are structural units with strong structural deformation. The Yishan Slope and the southern margin of the Yimeng Uplift are areas with very weak structural deformation. The advanced structures are generally characterized by a structural pattern of northeast high, south west and low. The sedimentary period of marine carbonate rocks on the Yishan Slope showed a tectonic framework of high northwest and low south east ( image 3 ).
[0049] The eastern area of the Sulige Gas Field is located on the northeast side of the Yishan Slope in the Ordos Basin structurally, and on the south side of the Yimeng Uplift. Geographically located in the east and north of Wushen Banner. The average well spacing in...
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