Synthetical analysis of the distribution and evolution of tectonics reveals that the Neocathaysian tectono-facies system controls the distribution of rocks and ore deposits in Mesozoic in the middle and lower reaches of the Yangtze River. The main tectonics of Neocathaysian tectono-facies system are large-scale NNE-trending folds and shearing compressive fault belt, distributing in left echelon, with two corresponding wrench shear structure, whose predecessors called Taishan-type and Dayishan-type tectonic belt, accompanied with NWW-trending structure delelopping well in the Yangtze River Basin. Therefore, in this paper, the Wuhan-Jiujiang-Dexing NWW-trending deep structural belt is called Yangtze River-type structure, which belongs to the Neocathaysian transversely tensioned structure of compressive zone.