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四川盆地高石梯—磨溪地区走滑断层识别
引用本文:邱泽华,周路,陈骁,关旭,吴勇,钱妤婕.四川盆地高石梯—磨溪地区走滑断层识别[J].石油地球物理勘探,2022,57(3):647-655.
作者姓名:邱泽华  周路  陈骁  关旭  吴勇  钱妤婕
作者单位:1. 西南石油大学天然气地质四川省重点实验室, 四川成都 610500;2. 西南石油大学地球科学与技术学院, 四川成都 610500;3. 中国石油西南油气田公司勘探开发研究院, 四川成都 610041
基金项目:国家自然科学基金项目“四川盆地东部多重滑脱构造变形系统及其控油气作用”(41430316);;国家科技重大专项“典型盆地深层油气输导格架建立与油气成藏分析”(2017ZX05008-004-008)联合资助;
摘    要:四川盆地高石梯—磨溪地区二叠系栖霞组不断发现天然气,油气勘探潜力巨大。张扭性走滑断层控制着油气分布,但目前对于走滑断层特征的研究较少,并且仅根据地震剖面识别走滑断层具有局限性。为此,从走滑断层形成的力学机制入手,分析构造样式及构造特征,并以海豚效应和丝带效应指导走滑断层识别;分析、对比多种地震属性优、缺点,优选最适合走滑断层识别的地震属性。研究认为:高石梯—磨溪地区走滑断层主要受里德尔剪切的单剪模式控制;剖面上表现为正花状构造、线状构造、“Y”字型构造及多期花状构造叠加等构造样式,具有断距小、层位错动不明显、以同相轴弯曲扰动为主的特征;平面上具有辫状构造、雁列状构造、马尾构造等多种构造样式,沿断层走向具海豚效应,沿断层倾向具丝带效应;基于波形相似性相干算法的地震属性分析识别走滑断层效果较差,曲率属性和蚂蚁体属性可较清晰地识别走滑断层平面展布特征。该方法可为其他同类地区走滑断层识别提供参考。

关 键 词:四川盆地  高石梯—磨溪地区  二叠系栖霞组  走滑断层  地震属性  构造样式  
收稿时间:2021-09-21

Identification of strike-slip faults in Gaoshiti-Moxi area of Sichuan Basin
QIU Zehua,ZHOU Lu,CHEN Xiao,GUAN Xu,WU Yong,QIAN Yujie.Identification of strike-slip faults in Gaoshiti-Moxi area of Sichuan Basin[J].Oil Geophysical Prospecting,2022,57(3):647-655.
Authors:QIU Zehua  ZHOU Lu  CHEN Xiao  GUAN Xu  WU Yong  QIAN Yujie
Affiliation:1. Sichuan Provincial Key Laboratory of Natural Gas Geology, Chengdu, Sichuan 610500, China;2. School of Geosciences and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China;3. Exploration and Development Research Institute, PetroChina Southwest Oil & Gas Field Company, Chengdu, Sichuan 610041, China
Abstract:Natural gas is continuously discovered in the Permian Qixia Formation in the Gaoshiti-Moxi area of the Sichuan Basin, and thus this area has great potential for oil and gas exploration. Transtensional strike-slip faults control the distribution of oil and gas, but there is little research on the characteristics of strike-slip faults, and it is insufficient to identify strike-slip faults only according to seismic profiles. Therefore, starting with the mecha-nical mechanism of the formation of strike-slip faults, this paper analyzes the structural styles and structural characteristics and guides the identification of strike-slip faults with the dolphin effect and ribbon effect. Moreover, the advantages and disadvantages of various seismic attributes are analyzed and compared, and the seismic attributes most suitable for strike-slip fault identification are selected. The study believes that the strike-slip faults in the Gaoshiti-Moxi area are mainly controlled by the single shear mode of Riedel shear. On the section, the structural styles include the positive flower structure, linear structure, Y-shaped structure, and the superposition of multi-stage flower structures, which are characterized by small fault displacement, unobvious horizon dislocation, and dominant event bending disturbance. On the plane, structural styles include the braided structure, en-echelon structure, and horsetail structure, and the dolphin effect and ribbon effect appear along the fault strike and the fault dipping direction, respectively. The seismic attribute ana-lysis by the waveform similarity-based coherence algorithm has a poor identification effect of strike-slip faults, while the curvature and ant body attributes can clearly identify the planar distribution characteristics of strike-slip faults. This method can provide a reference for the identification of strike-slip faults in other similar areas.
Keywords:Sichuan Basin  Gaoshiti-Moxi area  Permian Qixia Formation  strike-slip fault  seismic attributes  structural style  
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