[an error occurred while processing this directive] ������� 2015, 34(1) 187-193 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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PubMed
Article by Yu, Q. S.
Article by Zhang, F. X.
Article by Ceng, S. F.
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���ù�һ����֡�Theta map ����ʶ�𷽷��嶨�����˰�����Ѵ����ں�—�������—�׳Ƕ��ѵ�λ�ã���֤�˺ں�—�������—�׳Ƕ��ѵĴ���; ���ǰ���о��ɹ�����ص��ʵ����������Ϸ�����Ϊ�ں�—�������—�׳Ƕ����Ƕ������—�˰��ؿ������۵ؿ�Ĵ�ع���ֽ��ߣ������˰�����Ѵ����ɶ������—�˰��ؿ��ϵĹ��챡��λ�����ܼ�ѹ������ɵؿǹ���䶯�γɵľ�������Ѵ�; ���� Oasis Montaj �شŷ�����������˻�����������֤���������о�������ĵ��ʹ���ģ�͡�

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��esearch on geophysical field in northern part of Da Hinggan mountains
YU Qing-Shui, ZHANG Feng-Xu, ZENG Shao-Fa
College of Geo-exploration Science and Technology��Jilin University��Changchun 130026��China
Abstract:

According to the Normalized Differential and the Theta map fracture identification techniques��this article fixes the locations of the Da Hinggan mountains fracture zone and the Heihe - - Qiqihar - - Baicheng fracture�� It verifies the existence of the Heihe - -Qiqihar - -Baicheng fracture�� According to previous research results as well as related geological and geophysical data��we argue that the Heihe- - Qiqihar- - Baicheng fracture is the tectonic bounda- ry of Erguna- - Xing'an plot and Songnen massif�� While the Da Hinggan mountains fracture zone is a giant deep fault which is attributed to crustal tectonic movements squeezed by weak structures of the Erguna - - Xing'an plot�� Utilizing Oasis Montaj gravity and magnetic inversion software for human- computer interaction��we conclude a reasonable ge- ological structure model suitable for the research area��

Keywords: Da Hinggan mountains fracture zone   Heihe-Qiqihar-Baicheng fracture   geological structure model   Geotectonic boundary  
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