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准噶尔盆地基底构造分区的重磁异常分析

Analysis on Gravity-Magnetic Anomalies in Basement Geotectonic Divisions in Junggar Basin

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【作者】 赵俊猛马宗晋姚长利黎益仕刘占坡

【Author】 ZHAO Jun-meng1,2, MA Zong-jin2, YAO Chang-li3, LI Yi-shi4, LIU Zhan-po2 (1.Institute of Tibetan Plateau, CAS, Beijing 100085, China; 2.Institute of Geology, China Earthquake Administration, Beijing 100029, China; 3.China University of Geosciences, Beijing 100083, China; 4.China Earthquake Administration, Beijing 100036, China)

【机构】 中国科学院青藏高原研究所中国地震局地质研究所中国地质大学中国地震局中国地震局地质研究所 北京100085中国地震局地质研究所北京100029北京100083北京100036

【摘要】 利用准噶尔盆地及周边地区1∶200000重磁异常,采取多种处理与分析方法,在准噶尔盆地内共确定主要断裂48条,其中一级断裂7条、二级断裂6条、三级断裂35条。尤其是通过详细的资料处理,并结合盆地盖层沉积特点确定了基底南北、东西向断裂F6、F1的存在。研究认为,准噶尔盆地可划分为Ⅰ(南部)、Ⅱ(中部)、Ⅲ(北部)3个一级构造区,其中Ⅱ(中部)构造区可进一步划分为4个亚区并构成盆地内部的4个象限,而其中的每个象限又可划分出若干个次一级的构造单元。这4个象限的结构、密度分布、磁化强度各不相同,形成空间与时间上的差异特征。

【Abstract】 Based on the 1:200 000 gravitational and magnetic anomalies, the 48 faults in Junggar basin including 7 of first class, 6 of second class and 35 of third class have been determined, by means of multi-processing and analyses. In particular, the fault F6 in EW orientation and the fault F1 in SN orientation have been determined by detailed data processing and combining with crystalline basement deposition feature of the basin. The study shows that Junggar basin can be classified into such three first tectonic regions as Region Ⅰ (southern part), Region Ⅱ (middle part) and Region Ⅲ (northern part). The Region Ⅱ can be further divided into 4 sub-regions, forming a four-phase pattern. The each phase can be also divided into several further secondary geotectonic units. The structure, density and magnetic intensity are different in each phase, composing some differences in time and space.

  • 【文献出处】 新疆石油地质 ,Xinjiang Petroleum Geology , 编辑部邮箱 ,2008年01期
  • 【分类号】P544.4
  • 【被引频次】27
  • 【下载频次】594
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