Special Oil & Gas Reservoirs ›› 2024, Vol. 32 ›› Issue (5): 66-75.DOI: 10.3969/j.issn.1006-6535.2025.05.008

Previous Articles     Next Articles

Geological characteristics of the second member of the Permian Wujiaping Formation in the Longmenba Section, eastern Chongqing

CHEN Miankun1, XU Lulu2, YAO Mingjun1, LIU Zaoxue2, WEN Yaru2   

  1. 1. Sinopec Jianghan Oilfield Company, Wuhan, Hubei 430074, China;
    2. Hubei Geological Survey, Wuhan, Hubei 430034, China
  • Received:2024-04-14 Revised:2025-07-20 Online:2025-09-25 Published:2025-10-30

Abstract: Currently, commercial development of shale gas has been achieved in the Second Member of the Permian Wujiaping Formation (referred to as Wu 2 Member) in the Hongxing Area within the Liangping-Kaijiang Trough in eastern Chongqing. However, research on shale gas accumulation conditions in the north-central part of the western Hubei Trough remains insufficient. Therefore, through detailed measurement and sample analysis of the Permian Wu 2 Member stratigraphic section in Longmenba, Fengjie County, eastern Chongqing, the characteristics of the Wu 2 Member shale reservoir were clarified and the shale gas exploration potential areas in western Hubei-eastern Chongqing were predicted. The results indicate that the thickness of organic-rich shale in the Wu 2 Member reaches 29.3 m and can be divided into five sub-layers. The organic-rich intervals are sub-layers 1, 3, 4 and 5, mainly composed of black argillaceous siliceous rocks interbedded with siliceous shale, with increasing calcareous content upward in the formation; sub-layers 1 and 3 are volcanic ash-dense intervals,with the first appearance of the conodont C.wangi near the top of bed 101 as the boundary between the Wujiapingian and Changxingian stages; the organic-rich intervals were deposited in a humid,semi-humid,semi-arid climate with anoxic bottom water and high productivity paleoenvironments. The average TOC is 6.34%, characterizing a carbon riched, silicon riched, low porosity, low permeability reservoir. Compared with the Hongxing Area and the Enshi Area, although the Wu 2 Member has a relatively shallow (mostly less than 2 000 m) burial depth, it has large thickness (about 30 m) and high TOC (greater than 4.00%), thus still possessing good shale gas accumulation potential. The research results can provide geological basis for the construction of a shale gas exploration and development demonstration area in western Hubei-eastem Chongqing.

Key words: black shale, reservoir characteristics, accumulation potential, Wujiaping Formation, eastern Chongqing

CLC Number: