The Range and Evolution Model of the Xiang-E Submarine Uplifts at the Ordovician-Silurian Transition: Evidence from Black Shale Graptolites

被引:0
作者
Zhou, Zhi [1 ,2 ,3 ,4 ]
Zhou, Hui [2 ,3 ,4 ]
Jiang, Zhenxue [1 ]
Li, Shizhen [2 ,3 ,4 ]
Bao, Shujing [1 ,2 ,3 ,4 ]
Xu, Guihong [5 ]
机构
[1] China Univ Petr, Inst Unconvent Nat Gas Res, Beijing 102249, Peoples R China
[2] China Geol Survey, Oil & Gas Resources Survey Ctr, Beijing 100083, Peoples R China
[3] State Key Lab Continental Shale Oil, Beijing 100083, Peoples R China
[4] China Geol Survey, Key Lab Unconvent Petr Geol, Beijing 100083, Peoples R China
[5] Beijing CAS Geophys Energy Technol Co Ltd, Beijing 100078, Peoples R China
关键词
Ordovician; Silurian; Wufeng Formation; Longmaxi Formation; Xiang-E submarine uplifts; shale gas; FORMATION-LONGMAXI FORMATION; SOUTH CHINA; YANGTZE BLOCK; WUFENG; BENTONITE; CATHAYSIA; BASIN; GAS;
D O I
10.3390/jmse13040739
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
Accurately delineating the range of the Xiang-E submarine uplifts is the key to the exploration and development of Silurian shale gas in the Western Hunan-Hubei region. Based on the graptolite stratigraphic division of Well JD1 in Jianshi area, Hubei Province, and combined with the GBDB online database (Geobiodiversity Database), the study compared the shale graptolite sequences of the Wufeng Formation and Longmaxi Formation from 23 profile points and 11 wells which cross the Ordovician-Silurian boundary. The range of the Xiang-E submarine uplift was delineated, and its evolution model and formation mechanism at the Ordovician-Silurian transition were discussed. The graptolite stratigraphic correlation results of drillings and profiles confirmed the development of submarine uplifts in the Western Hunan-Hubei region at the Ordovician-Silurian transition-Xiang-E submarine uplift. Under the joint control of the Guangxi movement and the global sea-level variation caused by the condensation and melting of polar glaciers, the overall evolution of the Xiang-E submarine uplift is characterized by continuous uplift from the Katian Age to the early Rhuddanian Age, with the influence gradually expanding, and then gradually shrinking back in the middle and late Rhuddanian Age. The initial form of the Xiang-E submarine uplift may have originated from the Guangxi movement, and the global sea-level variation caused by polar glacier condensation and melting is the main controlling factor for the changes in its influence range. Within the submarine uplifts range, the Wufeng-Longmaxi Formations generally lack at least two graptolite zone organic-rich shales in the WF2-LM4, and the shale gas reservoir has a poor hydrocarbon generation material foundation, posing a high risk for shale gas exploration. The Silurian in Xianfeng, Lichuan, Yichang of Hubei and Wushan of Chongqing has good potential for shale gas exploration and development.
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页数:15
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