Differential evolution of pore fluid pressure in the Sinian carbonate reservoirs of the central and eastern Sichuan Basin, China: Implication for gas preservation and destruction

IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2024-07-17 DOI:10.1002/gj.5023
Jiaxu Chen, Changwei Chen, Zhiliang He, Xiaowen Guo, Huahui Zhu, Ze Tao, Tao Luo, Dianwei Zhang, Ziming Sun
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Abstract

Trillions of cubic meters of gas reserve have been found in the Sinian Dengying carbonate reservoirs with normal pressure in the central Sichuan Basin, while no industrial gas reservoir have been detected in the Sinian Dengying reservoir with normal pressure in the eastern Sichuan Basin. The pore fluid pressure of gas reservoir is usually closely related to total gas content. To investigate the pore fluid pressure evolution and its implication for gas reserve preservation in the Sinian Dengying reservoir of the central and eastern Sichuan Basin, we conducted a comprehensive analysis including fluid inclusion petrography, microthermometry and Raman spectroscopy. The timings of gas inclusions captured in the central and eastern Sichuan Basin occurred from 175 to 92 Ma and 191 to 183 Ma, respectively. The presence of two-phase vapour-solid bitumen inclusions with similar phase proportions in a single fluid inclusion assemblage of fluorite provides direct evidence of in situ oil cracking to gas. The widespread solid bitumen from the Sinian Dengying reservoir in the central Sichuan Basin indicates the existence of massive oil cracking, which results in the formation of overpressure in the reservoir. Pore fluid pressure evolution of the Sinian Dengying reservoir of the central Sichuan Basin experiences normal pressure stage (200–155 Ma), overpressure development stage (155–90 Ma) and overpressure release stage (90–0 Ma). The maximum pore fluid pressure and its corresponding pressure coefficient of the Sinian Dengying reservoir of the central Sichuan Basin are approximately 141.4 MPa and 1.95, respectively. The overpressure development stage reflects the processes of oil cracking and gas accumulation, and the overpressure release stage reflects the dissipation of some natural gas in the Sinian Dengying reservoir of the central Sichuan Basin. The pore fluid pressure of the Sinian Dengying reservoir in the eastern Sichuan Basin has maintained at normal pressure since 200 Ma, indicating that the gas reservoir was small during the oil cracking stage and natural gas completely leaked due to tectonic uplift.

中国四川盆地中部和东部新安江碳酸盐岩储层孔隙流体压力的差异演化:对天然气保存和破坏的影响
在四川盆地中部常压的中年登井碳酸盐岩储层中发现了数万亿立方米的天然气储量,而在四川盆地东部常压的中年登井储层中未发现工业气藏。气藏的孔隙流体压力通常与总含气量密切相关。为研究四川盆地中、东部中年登瀛储层孔隙流体压力演化及其对气藏保存的影响,我们进行了流体包裹体岩相学、微热学和拉曼光谱等综合分析。在四川盆地中部和东部捕获的气体包裹体的时间分别为175-92 Ma和191-183 Ma。在单一的萤石流体包裹体集合体中存在相比例相似的两相汽固沥青包裹体,为原地石油裂解为气体提供了直接证据。四川盆地中部的新安邓营储层中广泛存在的固体沥青表明存在大规模的石油裂解,导致储层中形成超压。四川盆地中部中年登瀛储层孔隙流体压力演化经历了常压阶段(200-155 Ma)、超压发育阶段(155-90 Ma)和超压释放阶段(90-0 Ma)。四川盆地中部新安邓营储层的最大孔隙流体压力及其相应的压力系数分别约为 141.4 兆帕和 1.95。超压发育阶段反映了四川盆地中部中年登瀛储层的石油裂解和天然气聚集过程,超压释放阶段反映了四川盆地中部中年登瀛储层中部分天然气的消散过程。四川盆地东部中年登瀛储层的孔隙流体压力自 200 Ma 以来一直保持常压,说明在石油裂解阶段气藏规模较小,构造隆起导致天然气完全泄漏。
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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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