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《Geophysical and Geochemical Exploration》 2002-02
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REDETERMINATION OF THE BOUNDARY BETWEEN CHINESE PLATFORM AND DA HINGGAN LING-MONGOLIAN PALEOZOIC GEOSYNCLINAL FOLDED BELT

ZHANG Zhen-fa 1,NIU Ying-zhi 1,CHANG Zhong-yao 2,GE Chang-bao 3 (1.Inner Mongolian No.1 Institute of Geophysical and Geochemical Exploration, Hohhot 010020, China; 2.Inner Mongolian Geological Survey, Hohhot 010020, China; 3.Division of Geology, Inne  
According to geophysical field characteristics, seismic sounding, magnetotelluric sounding and recent geological data, the boundary between Chinese platform and Da Hingganling-Mongolian Paleozoic geosynclinal folded belt lies along Xar Moron River? Wenduermiaobei?Baiyinyanzhongxingaobaobei-Baoyintubei-Qeh-Talin tectonic line, and from Talin eastward, the geosyncline-platform boundary stretches along the northern boundary of Tarim platform; from Xar Moron River eastward, the geosyncline-platform boundary pinches out on the southwestern edge of Songliao Precambrian landmass.
【CateGory Index】: P631.4
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