摘要
A long peroid magnetotelluric profile along the Luqu-Longmenshan-Hechuan has been finished which helps to study the crust-mantle electrical resisitivity structure in Longmenshan and its adjacent area,Institutive and reasonable 2-D inversion algorithm under sector boundary was adopted.The results of this profile has shown the crust-mantle high resistance belt in Ruergai,Longmenshan,central Sichuan and low resistance belt in Songpan from northwest to southeast.Longmenshan crust-mantle high resistance block shows up as wedge-shaped high resistance block stretching to northwest under the Longmenshan thrust belt.Due to bi-directional compression of East margin of Qinghai-Tibet plateau and upper Yangtze plate,Crust materials of Songpan-Ganzi massifs thrust to Longmenshan,and middle-lower crust and upper mantle slides toward southwest,presenting a trend that west margin of upper Yangtze plate in shape of wedge inserting into east brim of Qinghai-Tibet Plateau.It was initially thought that Songpan crust-mantle ductile shear belt is regarded as the west margin deep boundary of upper Yangtze plate since Mesozoic-Cenozoic Era.