复杂断块地层构造裂缝表征及应力分析——以川中地区灯影组二段为例

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-03-24 DOI:10.1155/gfl/6622597
Yu Fan, Jianhua Guo, Xu Yang, Xihui Hu, Xinyu Shen, Qiutong Wang, Yijia Tang
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引用次数: 0

摘要

四川盆地坪坦 1 井区内的登瀛层是勘探开发的重要气藏。该储层位于复杂的断块构造中,具有多级断层演化的特点,导致构造裂缝分布复杂,对油气的聚集和运移至关重要。本研究建立了一个地质模型来描述在该地区观察到的断层模式,并对古构造应力场进行了数值模拟。此外,我们还结合岩石断裂标准以及应变和表面能理论,对构造断裂进行了定量预测。我们的研究结果表明,研究区域的构造断裂主要由剪切断裂组成,主要发育低角度和斜向断裂,其次是高角度断裂。这些断裂一般呈北北西(NNW)、东北(NE)、近东西(EW)和近南北(SN)走向。燕山-喜马拉雅时期形成的大多数断裂被确定为有效断裂。喜马拉雅构造活动时期记录到的最大和最小主应力值分别为 150-180 兆帕和 120-150 兆帕。断层对构造应力的分布有很大影响,应力集中通常发生在断层附近。构造应力与埋藏深度之间存在明显的相关性,埋藏深度越浅,应力水平越低。此外,断裂的线性密度从断层核心向外围逐渐减小,并进一步减小到远离断层的区域。在这三个区域,断裂主要按照高角度、斜角度和低角度的顺序发展。这项研究加深了我们对登瀛组断裂动态的了解,对该地区的地质力学性质和潜在的油气开采策略提供了宝贵的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Tectonic Fracture Characterization and Stress Analysis in Complex Fault Block Formations: A Case Study in the Second Member of Dengying Formation in Central Sichuan

Tectonic Fracture Characterization and Stress Analysis in Complex Fault Block Formations: A Case Study in the Second Member of Dengying Formation in Central Sichuan

The Dengying Formation within Pengtan 1 well area in the Sichuan Basin is a vital gas reservoir for exploration and development. The reservoir is situated in a complex fault block structure characterized by multistage fault evolution, leading to a complicated distribution of tectonic fractures crucial for the accumulation and migration of oil and gas. This study establishes a geological model to describe the fault patterns observed in the region and conducts numerical simulations of the paleotectonic stress field. Moreover, we combine rock fracture criteria and strain and surface energy theories to predict tectonic fractures quantitatively. Our findings indicate that the tectonic fractures in the study area predominantly consist of shear fractures, with primary development of low-angle and oblique fractures and, to a lesser extent, high-angle fractures. These fractures generally exhibit trends in the north–northwest (NNW), northeast (NE), nearly east–west (EW), and nearly south–north (SN) directions. Most fractures formed during the Yanshanian–Himalayan period are identified as effective fractures. The maximum and minimum principal stress values recorded for the Himalayan period of tectonic activity were 150–180 and 120–150 MPa, respectively. Faults significantly influence the distribution of tectonic stress, and stress concentration usually occurs near the fault. A significant correlation exists between tectonic stress and burial depth, exhibiting lower stress levels at shallower depths. In addition, the linear density of fractures gradually decreases from the fault core to its periphery and further decreases to areas far away from the fault. In these three regions, fractures mainly develop in the order of high angle, oblique, and low angle. This study enhances our understanding of the fracture dynamics within the Dengying Formation, contributing valuable insights into the region’s geomechanical properties and potential hydrocarbon exploitation strategies.

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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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