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《Chinese Journal of Geophysics》 2011-02
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A research on the geoelectrical banding characteristics of the bottom of the Mesozoic-Cenozoic basin groups in the Northwest of the Da Hinggan Ling fault

LIU Cai,YANG Bao-Jun~*,WANG Zhao-Guo,LIU Yang, WANG Dian,FENG Xuan,LU Qi,WANG Shi-Yu Geo-Kxploration Science and Technology Institute,Jilin University,Changchun 130026,China  
The structures of the Mesozoic-Cenozoic basin groups (Hailar basin,Genhe basin, Mohe basin) lying in the Northwest of the Da Hinggan Ling fault are controlled by the Da Hinggan Ling fault and the Derbugan fault,and the regional tectonic stress field of the Mongol-Okhotsk suture zone in the Northwest of the basin groups,the Xilamulunhe-Yanji suture zone in their southern part,even the movements of the western Pacific plate and the Indian plate far away from the basins and the micro-plates collage zones in the middle and west of Heilongjiang province make a superimposed effect to the bottom of the basin groups,both of which produce the complex deep structure features.Using the geoelectrical structure of the four MT sections (about 1000 km,94 survey points) carried out along the basin groups in this paper,the banding characteristic of geoelectrical structure of the bottom of the basin groups from Northwest to Southeast is obtained."The effect of the low electrical resistance" is introduced to describe the change of the physical feature of the basin bottom.The comprehensive analysis shows that the electrical structure of the bottom of the basin groups perhaps continue to evolve by the effect of the asthenosphere hot material.
【Fund】: 国家973计划课题(2009CB219301);; 国家自然科学基金(40974054);; 博士点基金(200801830042);; 国家科技支撑计划(2008-2012);; 公益性行业科研专项项目(201011078);; 油页岩勘探开发利用产学研用合作创新研究项目(OSP-02、OSR-02)资助
【CateGory Index】: P631.3
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