The draw thrust sheet tectonics is a new viewpoint put forward by Yang Zhihua during his study on development and evolution of the Qinling orogenic belt.
抽拉—逆冲岩片构造是杨志华等在研究秦岭造山带过程中提出的一种关于大陆造山带形成与演化的全新构造观。
The occurrence characteristics, size and position of all the deposits in the Xicheng orefield are completely controlled by the Choula (draw) -thrust sheet.
西成矿田中所有矿床的产出特征、规模和部位完全受抽拉—逆冲岩片构造的控制。
Hong, R. H. (1994) Analysis of deformation fabrics in the Sani thrust sheet and the Chuhuangkeng anticline of western Taiwan. Petroleum Geology of Taiwan, 29, 105-126.
洪日豪(1994)台湾西部三义逆冲断块及出磺坑背斜的变形组构分析。台湾石油地质，第29号，第105 - 126页。
The Parefin 4 chromite claims near the northern end of the Csardas thrust again indicate the eastward extension of the thinning ultrabasic sheet from Railway Block.
靠近萨达斯冲断层北端的帕勒芬4铬矿区又表明从铁路段向东超基性岩席减薄的情况。
The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.
其主要类型有席状逆冲构造、侏罗山式褶皱推覆构造、楔状推覆构造及剪切褶皱逆冲构造等。
The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.
其主要类型有席状逆冲构造、侏罗山式褶皱推覆构造、楔状推覆构造及剪切褶皱逆冲构造等。
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