期刊文献+
共找到1篇文章
< 1 >
每页显示 20 50 100
ANISOTROPIC FEATURE OF QIANGTANG MASSIF TEXTURE 被引量:4
1
作者 Yang Xingke,Liu Chiyang,Sun Dongsheng,Wang Dingyi,Lu Bing 《地学前缘》 EI CAS CSCD 2000年第S1期137-138,共2页
Qiangtang Massif is located in the hinterland of Qinghai—Tibet plateau, which belong to the mid\|east section of Tethys Tectonic Domain.1 Features of the whole texture and structure of Qiangtang massif By synthetic a... Qiangtang Massif is located in the hinterland of Qinghai—Tibet plateau, which belong to the mid\|east section of Tethys Tectonic Domain.1 Features of the whole texture and structure of Qiangtang massif By synthetic analysis of gravity,magnetic field,MT,seismic surveying,etc. Geophysical data, the massif, lied in the tectonic setting and geodynamic setting mingled by the south,north tectonic belts, have the features of massif,basin and tectonic belt three forming an organic whole,multi\|degree coupling in plane and section with division of region in south\|north trend,division of block\|fault in east\|west trend,division of sphere\|layer in vertical direction. (1) Belting in south\|north trend: Qiangtang massif could be divided into four units from north to south, that is north edge doming zone, west part doming area,Qiangtang Basin and south edge doming zone. Qiangtang Basin also can be divided into four tectonic units—north Qiangtang down\|warping region, middle downing zone, south Qiangtang down\|warping and east part slope region. The near east\|west trend tectonic zones are well developed. There is aero\|magnetic anomaly distributed in belting with east\|west trend but also concentrated in section. Gravity anomaly is high in the south\|west part and low in the northeast part. Inter\|crust low resistance layer alternately distributed with high and low belting of sou th\|north trend in plane. 展开更多
关键词 Qinghai—Tibet plateau QIANGTANG MASSIF TEXTURE anisotropism belting of south\|north TREND block\|faulting of east\|west TREND vertical sphere\|layering deep TEXTURE
下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部