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青藏高原北缘重力场特征与深部地壳构造

STUDY ON THE GRAVITY FIELD AND DEEP-SEATED CRUSTAL STRUCTURE AT THE ALTUN MTS-THE QILIAN MTS AREA

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【作者】 孟令顺崔军文

【Author】 MENG Ling_shun 1,CUI Jun_wen 2 (1.Changchun University of Science and Technology, Changchun 130026, China; 2.Institute of Geology, Chinese Academy of Geological Sciences (CAGS), Beijing 100037, China)

【机构】 长春科技大学地球探测与信息技术学院!吉林长春130026中国地质科学院地质研究所!北京100037

【摘要】 以老茫崖—阿尔干和格尔木—额济纳旗 2条 1∶5 0万实测重力剖面数据为基础 ,研究了青藏高原北缘的重力场特征 ,划分了 5个地质构造单元 ,计算并分析了研究区Airry均衡异常 ,推测阿尔金断裂带和北祁连断裂带为青藏高原北缘的动力边界。

【Abstract】 Based upon the 1∶500 000 gravity profiles of Laomangai-Argan, a study has been made on the gravity field features of the Qinghai-Tibet plateau′s north margin. This area can be divided into five geo-tectonic units. The Airy isostatic anomaly in this area has been calculated and analyzed. It is speculated that the Altun and the North Qilian fault zone are considered to be the dynamic boundary of the northern margin of the Qinghai-Tibet plateau.

  • 【文献出处】 长春科技大学学报 ,JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY , 编辑部邮箱 ,2000年02期
  • 【分类号】P312
  • 【被引频次】10
  • 【下载频次】238
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