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地球物理场特征、地震测深、大地电磁测深和最新地质资料表明 ,中华地台与兴蒙古生代地槽褶皱系的界线位于西拉木伦河—温都尔庙北—白音敖包北—宝音图北—策克—塔林构造线 ,从塔林向西 ,槽台界线沿塔里木地台北界延伸 ;从西拉木伦河向东 ,槽台界线尖灭在松辽前寒武陆块西南缘
The geophysical field characteristics, seismic sounding, geomagnetic sounding and the latest geologic data show that the boundary line between the Chinese platform and the Xingmou Paleozoic geosynclinal fold system is located in the north of the west Brahim - Pointing diagram North - Ceke - Tallinn tectonic line, from Tallinn west, trough boundary line along the northern boundary of Tarim platform extends; west of Xylong Mulun River, trough platform boundary line in the Songliao Precambrian block southwest edge