Lithofacies paleogeography and exploration significance of Sinian Doushantuo depositional stage in the middle-upper Yangtze region, Sichuan Basin, SW China

• Published in: Petroleum exploration and development Vol. 46; no. 1; pp. 41 - 53
• Main Authors: WANG, Zecheng, LIU, Jingjiang, JIANG, Hua, HUANG, Shipeng, WANG, Kun, XU, Zhengyu, JIANG, Qingchun, SHI, Shuyuan, REN, Mengyi, WANG, Tianyu
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-02-2019; KeAi Communications Co., Ltd
• Subjects: black shale; carbonate platform; Doushantuo Formation; lithofacies paleogeography; marginal sag; paleouplift; Sichuan Basin; Sinian; source rock; Sichuan Basin; black shale; source rock; lithofacies paleogeography; Sinian; paleouplift; carbonate platform; marginal sag; Doushantuo Formation
• ISSN: 1876-3804; 1876-3804
• DOI: 10.1016/S1876-3804(19)30004-7

In recent years, natural gas exploration in the Sinian Dengying Formation and shale gas exploration in Doushantuo Formation have made major breakthroughs in the Sichuan Basin and its adjacent areas. However, the sedimentary background of the Doushantuo Formation hasn't been studied systematically. The lithofacies paleogeographic pattern, sedimentary environment, sedimentary evolution and distribution of source rocks during the depositional stage of Doushantuo Formation were systematically analyzed by using a large amount of outcrop data, and a small amount of drilling and seismic data. (1) The sedimentary sequence and stratigraphic distribution of the Sinian Doushantuo Formation in the middle-upper Yangtze region were controlled by paleouplifts and marginal sags. The Doushantuo Formation in the paleouplift region was overlayed with thin thickness, including shore facies, mixed continental shelf facies and atypical carbonate platform facies. The marginal sag had complete strata and large thickness, and developed deep water shelf facies and restricted basin facies. (2) The Doushantuo Formation is divided into four members from bottom to top, and the sedimentary sequence is a complete sedimentary cycle of transgression–high position–regression. The first member is atypical carbonate gentle slope deposit in the early stage of the transgression, the second member is shore-mixed shelf deposit in the extensive transgression period, and the third member is atypical restricted–open sea platform deposit of the high position of the transgression. (3) The second member has organic-rich black shale developed with stable distribution and large thickness, which is an important source rock interval and major shale gas interval. The third member is characterized by microbial carbonate rock and has good storage conditions which is conducive to the accumulation of natural gas, phosphate and other mineral resources, so it is a new area worthy of attention. The Qinling trough and western Hubei trough are favorable areas for exploration of natural gas (including shale gas) and mineral resources such as phosphate and manganese ore.