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应用地球物理  2024, Vol. 21 Issue (4): 869-877    DOI: 10.1007/s11770-024-1150-3
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高精度重力在断裂识别中的应用——以准东米泉地区为例
江宁,李竹强*,王尹,包怡,王军*
1.江苏华东八一四地球物理勘查有限公司,江苏南京 210007;2.江苏省地质局 江苏南京 210001;3.中国石化胜利油田分公司勘探开发研究院,山东东营 257000;4.中国矿业大学资源与地球科学学院,江苏徐州 221116;5.中石化石油物探技术研究院有限公司,江苏南京 211103
Application of high-precision gravity in fracture identification: a case study of the Miquan region of the Junggar Basin
Jiang Ning, Li Zhu-qiang*, Wang Yin, Bao Yi, and Wang Jun*
1. Jiangsu East China 814 Geophysical Exploration Co., Ltd., Nanjing 210007, Jiangsu, China 2. Jiangsu Geological Bureau, Nanjing 210001, Jiangsu, China 3. Exploration and Development Research Institute, Shengli Oilfield Company, SINOPEC, Dongying 257000, China 4. School of Resources and Geosciences, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China 5. SINOPEC Geophysical Research Institute Co. Ltd, SINOPEC, Nanjing Jiangsu 211103, China
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摘要 重力梯度异常带是由于断层两侧密度差异所造成的。追踪重力水平总梯度极值点能够对断层位置刻画和描述。然而对于一些埋深较大的深部断层及埋深适中的次级断层,刻画比较困难。本文采用重力水平总梯度倾斜角“增强”的方法,以实现弱异常的提取,识别出更多的断层信息。该方法在米泉地区预测出5条区域深断层和6条次级断层。断层平面展布近北东东向,向西南方向呈喇叭状散开,而向北东方向收敛。因此,利用重力资料进行的断裂预测结果,对该区构造的深化认识具有重要的辅助作用。
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关键词断裂识别   重力异常   重力水平总梯度   重力倾斜角   米泉地区     
Abstract: The gravity gradient anomaly zone is produced due to density differences on both sides of a fault. Tracking of extreme points enables the characterization and description of fault locations. However, for some deep-seated faults with large burial depths and secondary faults with moderate burial depths, the gravity horizontal total gradient anomaly must be enhanced using the concept of dip angle to strengthen the weak anomaly extraction for the identification of more fault information. This method was used to predict five regional deep-seated faults and six secondary faults in the Miquan region. The fracture plane extends in a near north-northeast direction; that is, it mostly expands out of the study area, spreads out in a trumpet shape to the southwest, and converges to the northeast. Fracture activity is an important factor in controlling structural units or local structures. The Miquan block is located in a complex structural zone in front of the Bogeda Mountains, which have very complex surface and subsurface geological conditions, and seismic data are unideal. Therefore, fracture prediction results using gravity data are important in-depth understanding of the structure in this area.
Key wordsfracture identification   gravity anomaly   gravity level total gradient   gravity tilt angle   Miquan region   
收稿日期: 2024-08-11;
基金资助:This work was supported by the Sinopec Science and Technology Research Project (No. P22161 and No. 24029).
通讯作者: 李竹强(email: 276414616@qq.com), 王军(email: wangjun.swty@sinopec.com).     E-mail: 276414616@qq.com&wangjun.swty@sinopec.com
作者简介: Jiang Ning, Senior Engineer, is currently employed by Jiangsu East China 814 Geophysical Exploration Co., Ltd.. He mainly engages in the collection, processing, interpretation, and comprehensive research of non-seismic geophysical exploration related to oil, gas, and mineral resources, including gravity, magnetic, and electromagnetic methods. Email: 119846077@qq.com
引用本文:   
. 高精度重力在断裂识别中的应用——以准东米泉地区为例[J]. 应用地球物理, 2024, 21(4): 869-877.
. Application of high-precision gravity in fracture identification: a case study of the Miquan region of the Junggar Basin[J]. APPLIED GEOPHYSICS, 2024, 21(4): 869-877.
 
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