Shale Reservoir Characteristics and Development Control Factors of Lower Cambrian Qiongzhusi Formation in Sichuan Basin

Q2 Earth and Planetary Sciences Advances in Geosciences Pub Date : 2023-01-01 DOI:10.12677/ag.2023.139095
湛溪 陈
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Abstract

Recently, breakthroughs have been made in the down warping region SZY1 well, the “intracratonic sag” type Z201 well and the JS103 well in central Sichuan and southwest Sichuan, showing that the Lower Cambrian Qiongzhusi Formation in the Sichuan Basin has good exploration potential, but the differences and main controlling factors of different types of shale reservoirs are still unclear, and it is urgent to carry out comparative research on reservoir characteristics. Based on the data of three wells, this paper systematically compares and analyzes the petrology, geochemistry, re-servoir prosperities and crushability of different types of shale reservoirs in the Lower Cambrian Qiongzhusi Formation in the Sichuan Basin. The results show that the content of TOC and clay minerals in Cambrian shale of continent down warping region in northern Sichuan is higher, mainly organic matter pores and flaky clay mineral pores, the specific surface area and pore size are larger, and the pore development is mainly controlled by organic matter abundance and diagenesi. The black shale in the deep-water shelf facies of the intracratonic sag in central Sichuan basin had high TOC and gas content, mainly organic matter pores, and there was a good positive correlation be-tween porosity and organic matter abundance. The intracratonic sag shallow shelf facies sandy shale in southwest Sichuan has low TOC and low gas content, ntergranular pores, tiny crackand flaky clay minerals pores are the main pore types. The pore development is mainly controlled by diagenesis. The organic-rich shale of the Qiongzhusi Formation deposited in the deep-water shelf facies of the northern Sichuan basin and central Sichuan basin has certain similarities, with high TOC and high-quality shale sections dominated by organic pores. The intracratonic sag shallow shelf facies sandy shale in southwest Sichuan has low TOC, mainly inorganic pores, higher porosity and good crushability, and has certain exploration potential
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四川盆地下寒武统筇竹寺组页岩储层特征及发育控制因素
近年来,川中、川西南地区下弯区SZY1井、“克拉通内凹陷”型Z201井和JS103井取得突破性进展,表明四川盆地下寒武统筇竹寺组具有良好的勘探潜力,但不同类型页岩储层的差异及主控因素尚不清楚,储层特征的对比研究十分迫切。根据3口井资料,对四川盆地下寒武统筇竹寺组不同类型页岩储层的岩石学、地球化学、储层丰度和可破碎性进行了系统的比较分析。结果表明,川北陆相下隆起区寒武系页岩TOC和粘土矿物含量较高,主要为有机质孔隙和片状粘土矿物孔隙,比表面积和孔径较大,孔隙发育主要受有机质丰度和成岩作用控制。川中克拉通内凹陷深水陆架相黑色页岩TOC含量高,含气量大,以有机质孔隙为主,孔隙度与有机质丰度呈正相关。川西南克拉通内凹陷浅陆棚相砂质页岩TOC含量低,含气量低,孔隙类型主要为粒间孔、微裂纹孔和片状粘土矿物孔。孔隙发育主要受成岩作用控制。川北和川中深水陆架相筇竹司组富有机质页岩具有一定的相似性,具有高TOC和以有机孔隙为主的优质页岩剖面。川西南克拉通内凹陷浅陆棚相砂质页岩TOC含量低,孔隙以无机孔隙为主,孔隙度较高,可破碎性好,具有一定的勘探潜力
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来源期刊
Advances in Geosciences
Advances in Geosciences Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
3.70
自引率
0.00%
发文量
16
审稿时长
30 weeks
期刊介绍: Advances in Geosciences (ADGEO) is an international, interdisciplinary journal for fast publication of collections of short, but self-contained communications in the Earth, planetary and solar system sciences, published in separate volumes online with the option of a publication on paper (print-on-demand). The collections may include papers presented at scientific meetings (proceedings) or articles on a well defined topic compiled by individual editors or organizations (special publications). The evaluation of the manuscript is organized by Guest-Editors, i.e. either by the conveners of a session of a conference or by the organizers of a meeting or workshop or by editors appointed otherwise, and their chosen referees.
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