川西北双鱼石地区栖霞组储层成藏期次及流体演化

倪蕊; 马行陟; 陈勇; 冯艳伟; 鲁雪松; 宋一帆; 张辉; 范俊佳

doi:10.3799/dqkx.2022.403

Volume 48 Issue 2

Feb. 2023

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Article Navigation > Earth Science > 2023 > 48(2): 596-608

Ni Rui, Ma Xingzhi, Chen Yong, Feng Yanwei, Lu Xuesong, Song Yifan, Zhang Hui, Fan Junjia, 2023. Stages of Hydrocarbon Accumulationand Fluid Evolution of Qixia Reservoir in Shuangyushi Area, Northwest Sichuan Basin, China. Earth Science, 48(2): 596-608. doi: 10.3799/dqkx.2022.403

Citation:

Ni Rui, Ma Xingzhi, Chen Yong, Feng Yanwei, Lu Xuesong, Song Yifan, Zhang Hui, Fan Junjia, 2023. Stages of Hydrocarbon Accumulationand Fluid Evolution of Qixia Reservoir in Shuangyushi Area, Northwest Sichuan Basin, China. Earth Science, 48(2): 596-608. doi: 10.3799/dqkx.2022.403

Citation:

Ni Rui, Ma Xingzhi, Chen Yong, Feng Yanwei, Lu Xuesong, Song Yifan, Zhang Hui, Fan Junjia, 2023. Stages of Hydrocarbon Accumulationand Fluid Evolution of Qixia Reservoir in Shuangyushi Area, Northwest Sichuan Basin, China. Earth Science, 48(2): 596-608. doi: 10.3799/dqkx.2022.403

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Stages of Hydrocarbon Accumulationand Fluid Evolution of Qixia Reservoir in Shuangyushi Area, Northwest Sichuan Basin, China

doi: 10.3799/dqkx.2022.403

Ni Rui^{1, 2
,
,},
Ma Xingzhi³,
Chen Yong^{1, 2
,
,},
Feng Yanwei^{1, 2},
Lu Xuesong³,
Song Yifan^{1, 2},
Zhang Hui^{1, 2},
Fan Junjia³

1.
Shandong Provincial Key Laboratory of Deep Oil and Gas, Qingdao 266580, China
2.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
3.
Research Institute of Petroleum Exploration and Development, Beijing 100083, China

Received Date: 2022-11-15
Publish Date: 2023-02-25

Abstract

Abstract

Based on drilling core observation, combined polarizing microscopic observation forthin section, cathodoluminescence and fluid inclusion analysis, this paper discusses hydrocarbon accumulation and fluid evolution of Qixia Formation in Shuangyushi structure in northwestern Sichuan. There sults show that the upper reservoir of Qixia Formation of Shuangyushi structure in northwest Sichuan is sparry cloud limestone, and its fillings of diagenetic mineral can be divided into four stages, including early fine crystalline calcite, recrystallized calcite, quartz and albite filled in early limestone holes, and dolomite and calcite filled in pore cracks. Combined with the characteristics of fluid inclusions in different diagenetic stages and burial history analysis, it is found that study area was settled and accepted deposition from Permian to Middle Triassic, recrystallized calcite was formed due to the increase of burial depth and hydrothermal action associated with Emei taphrogeny.The early⁃middle Triassic to middle Jurassic lower Cambrian source rocks reached the peak of oil generation, which made the first stage of oil charged into Qixia Formation reservoir. Then the middle and lower Permian source rocks reached the peak of oil generation in the Early Jurassic and Early Cretaceous, that is, the second stage of oil charging. Quartz and albite were formed due to the charging of silica⁃rich hydrothermal fluid. At the same time, due to the burial depth and the transformation of hydrothermal fluid, part of the crude oil cracked into bitumen, and the ancient gas reservoir began to form gradually. The Longmenshan area experienced continuous thrust deformation in the middle and late Mesozoic from late Yanshanian to Himalayan, structural fractures were filled with dolomite and calcite. Methane and asphalt inclusions were captured in the veincalcite, and the ancient gas reservoirs were adjusted accordingly, which indicated the characteristics of early accumulation and late adjustment.
- Sichuan Basin,
- northwest Sichuan,
- Permian Qixia Formation,
- stages of hydrocarbon accumulation,
- fluid evolution,
- petroleum geology

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