Citation: | FENG Xukui, YANG Yu, ZHU Yadong, CUI Yongping, CHEN Hui, WU Furong, ZANG Dianguang, NI Hualing, WU Yulin, XU Baoliang, GUO Haiyang. 2024. Development characteristics, distribution patterns and favorable exploration zones of Permian reef shoals in Sichuan Basin. Sedimentary Geology and Tethyan Geology, 44(2): 278-294. doi: 10.19826/j.cnki.1009-3850.2023.01003 |
The exploration of carbonate rocks around the Permian Kaijiang-Liangping trough in the Sichuan Basin has achieved great success, but exploration has entered a bottleneck period in the past decade. In order to further deepen the understanding of Permian reef shoals and achieve new breakthroughs in large-scale exploration, based on drilling, logging, seismic, and geological data, a systematic study has been carried out on the Permian tectonic-sedimentary evolution characteristics and the distribution patterns of Permian reef shoals, and the favorable zones for further reef shoals exploration have been identified. Research shows that: (1) The shoal in the Qixia Formation tableland is controlled by the late Caledonian ladder-like annular erosion, featuring a ring-like distribution in the early, middle, and late stages. The Jiulong Mountain–Longgang region in northern Sichuan and the Yibin–Neijiang region in southern Sichuan have good conditions for the inner shoal formation of the ring-like tableland in the late stage of the second member of the Qixia Formation, with a low degree of exploration, needing further exploration in the next step. (2) The second stage of the Maokou Formation is the key period for the transformation of the sedimentary pattern of the Permian system. The sedimentation of the lower sub-member of the Maokou Formation was controlled by the residual landform of the Caledonian paleo-uplift, thus, the inner shoal is distributed in a ring belt. The ancient landform of the area to the upper sub-member of the Maokou Formation was affected by the uplift of the Emei mantle plume, so, the favorable sedimentary facies transformed into a "strip-like" distribution pattern trending northwest-southeast. The platform margin shoal of the upper sub-member of the Maokou Formation in the north slope region of Moxi is a major successor area of the Maokou Formation. (3) The platform margin reef shoals of the Changxing Formation migrated into the Kaijiang-Liangping trough to form multiple rows of reef shoals, which have superior source and reservoir distribution conditions, being a potential exploration area of the Permian system.
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Regional tectonic location map of Sichuan Basin(modified from Wei et al., 2019)
Stratigraphic distribution and sedimentary cycle characteristics of Permian–Triasic Feixianguan Formation in Wel GS18–Wel LT1, Sichuan Basinn
Distribution map of two-dimensional and three-dimensional seismic networks and typical drilling locations in the Sichuan Basin
Standard section of Permian seismic geological horizon interpretation in Sichuan Basin
Pre-sedimentary Paleogeologic map of the Permian system in Sichuan Basin
Planar distribution map of sedimentary landform in key stratum of Permian system in Sichuan Basin
Tectonic-sedimentary evolution and ref-shoal distribution model of the Permian–Triasic Feixianguan Formation in Sichuan Basin
Development characteristics of inner shoal and reservoir in Qixia Formation near the multi-stage erosion window of Lower Paleozoic in central and northwest Sichuan
Development characteristics of inner shoal and reservoir in the lower sub-member of Maokou Formation in Moxi region in central Sichuan
Development characteristics of inner shoal and reservoir in the upper sub-member of Maokou Formation in central and north Sichuan
Development characteristics of reef shoal of Changxing Formation in the western edge of Kaijiang-Liangping trough (within the trough)
Planar distribution of sedimentary facies in key stratum of Permian system in Sichuan Basin
Superposition map of the upper boundary tectonic setting of the Permian system and the favorable zones of the Permian reef-shoal in Sichuan Basin