库车前陆冲断带“石英桥”的发现及地质意义

王钊; 吕修祥; 张镭馨; 李峰; 欧阳思琪; 汪瑞

doi:10.3799/dqkx.2021.131

Volume 48 Issue 1

Jan. 2023

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Article Navigation > Earth Science > 2023 > 48(1): 342-358

Wang Zhao, Lü Xiuxiang, Zhang Leixin, Li Feng, Ouyang Siqi, Wang Rui, 2023. Discovery of 'Quartz Bridge' in Kuqa Foreland Thrust Belt and Its Geological Significance. Earth Science, 48(1): 342-358. doi: 10.3799/dqkx.2021.131

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Wang Zhao, Lü Xiuxiang, Zhang Leixin, Li Feng, Ouyang Siqi, Wang Rui, 2023. Discovery of "Quartz Bridge" in Kuqa Foreland Thrust Belt and Its Geological Significance. Earth Science, 48(1): 342-358. doi: 10.3799/dqkx.2021.131

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Discovery of "Quartz Bridge" in Kuqa Foreland Thrust Belt and Its Geological Significance

doi: 10.3799/dqkx.2021.131

Wang Zhao^{1, 2
,
,},
Lü Xiuxiang^{1
,
,},
Zhang Leixin³,
Li Feng¹,
Ouyang Siqi¹,
Wang Rui¹

1.
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China
2.
Consulting Center for Strategic Assessment, Academy of Military Science, Beijing 100097, China
3.
China National Petroleum News, Beijing 100011, China

Received Date: 2021-07-13
Available Online: 2023-02-01
Publish Date: 2023-01-25

Abstract

Abstract

Based on thin section and core data, quartz bridges in natural fractures of Cretaceous sandstones of the Keshen-Dabei area in the Kuqa foreland thrust belt were discovered by SEM, fluid inclusions and ion microprobe in-situ isotope. Quartz bridge is highly localized overgrowth accumulations that span fracture walls and is scattered on the fracture surface. Fluid inclusion assemblages sub-parallel to the fracture walls were observed in the quartz bridge. Their homogenization temperature range (150-176 ℃) is different from that of the fluid inclusions in quartz grains (90-120 ℃). Besides, the scope of δ¹⁸O_VSMOWvalues (17‰-21‰) does not overlap with that of quartz grain and quartz secondary enlargement (8‰-17‰). In the Cretaceous sandstone of the Keshen and Dabei area, quartz bridges are widespread in the hinge-parallel fractures. The formation of quartz bridge may be related to the extension during folding in the high-temperature at great depth and the migration of ¹⁸O-enriched water of Paleogene evaporates. The research of the quartz bridge is a frontier and practical field, which has great significance for reconstructing fracture opening history and preserving fracture physical properties.
- structural diagenesis,
- sandstone reservoir,
- natural fracture,
- cement,
- quartz bridge,
- petroleum geology

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References(56)

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Discovery of "Quartz Bridge" in Kuqa Foreland Thrust Belt and Its Geological Significance

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