• 责任者：Lv Guxian (Institute of Geomechanics ; Chinese Academy of Geological Sciences ; Beijing 100081 ; China) ; Cao Zhongqing
• 刊名：Geotectonica et Metallogenia
• 出版年：2011
• 卷期：35(4)
• 关键词：构造体系 ; structural system ; 成矿构造 ; metallotectonics ; 长江中下游成矿带 ; Metallogenic Belt of Middle and Lower Reaches of Yangtze River
• 页码：p.495-501
• 图表：7 illus., 27 refs.
• 分类号：0300
• 出版序号：20122187
• issnNo：ISSN1001-1552
• isbnNo：CN44-1595/P

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.