基性岩侵入对页岩矿物学特征的影响：以松辽盆地嫩江组为例

王岩; 荣辉; 焦养泉; 徐尚; 贾俊民; 曹民强; 程璇

doi:10.3799/dqkx.2020.177

Volume 46 Issue 6

Jun. 2021

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Article Navigation > Earth Science > 2021 > 46(6): 2188-2203

Wang Yan, Rong Hui, Jiao Yangquan, Xu Shang, Jia Junmin, Cao Minqiang, Cheng Xuan, 2021. Effects of Basic Intrusions on Shale Mineralogy: A Case Study from Nenjiang Formation in Songliao Basin. Earth Science, 46(6): 2188-2203. doi: 10.3799/dqkx.2020.177

Citation:

Wang Yan, Rong Hui, Jiao Yangquan, Xu Shang, Jia Junmin, Cao Minqiang, Cheng Xuan, 2021. Effects of Basic Intrusions on Shale Mineralogy: A Case Study from Nenjiang Formation in Songliao Basin. Earth Science, 46(6): 2188-2203. doi: 10.3799/dqkx.2020.177

Citation:

Wang Yan, Rong Hui, Jiao Yangquan, Xu Shang, Jia Junmin, Cao Minqiang, Cheng Xuan, 2021. Effects of Basic Intrusions on Shale Mineralogy: A Case Study from Nenjiang Formation in Songliao Basin. Earth Science, 46(6): 2188-2203. doi: 10.3799/dqkx.2020.177

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Effects of Basic Intrusions on Shale Mineralogy: A Case Study from Nenjiang Formation in Songliao Basin

doi: 10.3799/dqkx.2020.177

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Development Company of New Energy Sources of Liaohe Petroleum Exploration Bureau, CNPC, Panjin 124010, China

Received Date: 2020-03-30
Publish Date: 2021-06-15

Abstract

Abstract

Existing studies have shown that magmatic intrusion has effects on shale mineralogical characteristics, but the lack of a detailed anatomy of its scope and extent has restricted the accurate understanding of the influence mechanism of magmatic activities on shale mineralogical characteristics.Based on contact with diabase in southern Songliao basin shale as an object of the Nenjiang Formation, by means of core observation, XRD, polarizing microscope, and scanning electron microscopy, the contact zone shale is divided from the diabase intrusion from far and near into five zones: gray shale zone, 19 m thick; dark gray shale zone, thick 11 m; gray-black shale zone, 12.9 m thick; blue-gray shale zone, 1.5 m thick; gray-white shale zone, 2.2 m thick. Quartz content increases, with average contents of 27.0%, 33.6%, 51.7%, 56.7%, and 52.7%, respectively. The transition from terrestrial clastic quartz to high-temperature in-situ quartz (microcrystalline self-shaped quartz and microcrystalline spherical quartz), the recrystallization phenomenon intensified. The content of feldspar increases, with average contents of 8.8%, 12.0%, 14.0%, 15.1%, and 18.2%, respectively, which changes from semi-morphic to semi-self-shaped, and the recrystallization phenomenon intensified. The content of carbonate minerals decreases first and then increased, with the average contents of 9.0%, 10.0%, 7.5%, 4.5%, and 6.0%, respectively. The shape of siderite and calcite changes from self-shaped to colloidal and veined. The pyrite content gradually decreases, with average contents of 5.4%, 3.5%, 1.0%, 0%, and 0%, respectively, and transformed from strawberry-like and self-shaped to other-shaped granular. The clay mineral content gradually decreases, with average contents of 46.0%, 36.5%, 22.5%, 20.1%, and 19.0%, respectively, transformed from platy montmorillonite to floc illite.The results show that the intrusion of basic rock into shale not only accelerates the diagenetic evolution of shale, but also increases the brittle minerals and decreases the plastic minerals, which can improve the brittleness and compressibility of shale reservoirs but weaken the ability of shale gas to exist.
- basic intrusion,
- shale,
- Nenjiang Formation,
- Songliao basin,
- petroleum geology

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References(113)

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