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准噶尔盆地南缘盆地轮廓和构造属性及页岩气战略选区的重磁电勘探研究
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  • 英文篇名:Study on the shape and structural properties of the southern margin of Junggar Basin and the potential shale-gas strategic deposit with integrated geophysical methods
  • 作者:屈栓柱 ; 唐宝山 ; 张海珠 ; 叶高峰 ; 刘志龙
  • 英文作者:QU Shuanzhu;TANG Baoshan;ZHANG Haizhu;YE Gaofeng;LIU Zhilong;Geophysical and Geochemical Prospecting Party, Xinjiang Bureau of Geology and Mineral Resources;Geophysical Exploration Brigade of Hubei Geological Bureau;School of Geophysics and Information Technology, China University of Geosciences;Tianjin Geothermal Exploration and Development—Designing Institute;
  • 关键词:准噶尔盆地南缘 ; 综合地球物理方法 ; 页岩气 ; 大地电磁测深 ; 电阻率模型
  • 英文关键词:The southern margin of Junggar Basin;;integrated geophysical methods;;shale-gas;;magnetotellurics;;resistivity models
  • 中文刊名:地质论评
  • 英文刊名:Geological Review
  • 机构:新疆维吾尔自治区地质矿产勘查开发局地球物理化学探矿大队;湖北省地质局地球物理勘探大队;中国地质大学(北京)地球物理与信息技术学院;天津地热勘查开发设计院;
  • 出版日期:2019-09-15
  • 出版单位:地质论评
  • 年:2019
  • 期:05
  • 基金:中央返还两权价款项目“新疆乌鲁木齐市米东区页岩气战略选区调查”(编号:N16-2-LQ28)的成果~~
  • 语种:中文;
  • 页:252-262
  • 页数:11
  • CN:11-1952/P
  • ISSN:0371-5736
  • 分类号:P618.13;P631
摘要
准噶尔盆地油气资源丰富,位于准噶尔盆地与北天山结合部位的准噶尔盆地南缘,构造复杂,地震方法应用效果不理想,因此利用综合地球物理方法圈定研究区页岩气产出层位二叠系芦草沟组的分布深度与范围。通过200块岩石标本物性测量,获得了研究区主要地层密度、磁化率、极化率及电阻率等物性参数:研究区主要为沉积岩系,磁性普遍较弱,其中二叠系地层三叠系地层磁性小;各地层密度差异不大,其中砂岩密度常见值2.61×10~(3 )kg/m~3、泥岩密度常见值2.56×10~(3 )kg/m~3、页岩密度常见值2.54×10~(3 )kg/m~3;各地层电性特征差异较大,电阻率特征呈现如下关系:砂岩>泥岩>页岩。对实测重力、磁法、大地电磁测深等地球物理数据进行处理及反演,得到了研究区布格重力异常平面等值线图、磁异常平面等值线图及大地电磁三维反演电阻率结构模型图。研究区东南部主要表现为高布格重力异常、负磁异常特征,布格重力异常峰值为9.5×10~(-5 )m/s~2,磁异常峰值为-100 nT;西北部主要表现为低布格重力异常、正磁异常特征,布格重力异常峰值为-12×10~(-5 )m/s~2,磁异常峰值280 nT。MT三维反演结果显示芦草沟组a、b段分别为较高阻和中低阻。芦草沟组总体表现为中低重力、中低电阻、低磁异常特征。结合地质资料,建立了重磁电综合解释地质剖面。根据断裂破碎带表现为低重力、低电阻、低磁异常特征,新推断出研究区8条逆断层,并进一步推断了研究区芦草沟组地层空间展布特征,为下一步勘探井位论证提供了地球物理依据。
        The Junggar basin is riched in oil and gas resources. Its southern margin,which located between the Junggar basin and the northern Tianshan Mountains,is geologically complicated,which makes seismic methods inapplicable. Thus,non-seismic geophysical methods were employed to determine geometrical features of the Lucaogou Formation of Permian which was supposed to be potential shale-gas deposit. With 200 pieces of rock samples of main rocks showed in research area, some geophysical properties, such as density, magnetic susceptibility,polarizability and resistivity were measured,and some statistically conclusions were obtained. The study area is dominated by sedimentary rocks,whose magnetic is generally weak. The magnetic of Permian strata is lower than the Triassic ones. The density difference of main strata is insignificant with average values of 2. 61 x 10~3 kg/m~3,2. 56 x 10~3 kg/m~3 and 2. 54 x 10~3 kg/m~3 of sandstones,mudstones and shales respectively. However,the resistivity difference of these rocks is large enough,and an obvious resistivity relationship of sandstone > mudstone> shale can be concluded. The gravity,magnetic and magnetotelluric sounding data were collected in the research area. After careful data processing and inversion,the Bouguer gravity and magnetic anomalies in map view and three-dimensional resistivity model were produced. The southeastern part of research area characterized by high Bouguer gravity anomaly and negative magnetic anomaly with their peak values of 9. 5 x 10~(-5) m/s~2 and-100 nT respectively. In contrast,the northwestern part showed low Bouguer gravity anomaly and positive magnetic anomaly with their values of -12 × 10~(-5) m/s~2 and 280 n T respectively. Integrated with geological data,the a and b parts of target layer of the Lucaogou Formation show relatively high and medium to low resistivity in the three-dimensional resistivity model respectively. The strata of research area were deduced by integrated interpretation of gravity,magnetic data and resistivity model. Furthermore,eight thrust faults were deduced since faults are characterized with low resistivity,low gravity and low magnetic anomaly. Based on these new deduced thrust faults in the study area,the spatial distribution of the Lucaogou Formation was deduced,with which the positions of exploration wells were suggested.
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