• 责任者：Wang Yongjiang (China Aero Geophysical Survey and Remote Sensing Center for Land and Resources ; Beijing 100083 ; China) ; Geng Shufang
• 刊名：Geology in China
• 出版年：2009
• 卷期：36(3)
• 关键词：大地构造 ; tectonics ; 遥感 ; remote sensing ; 成矿规律 ; metallogenic regularity ; 塔里木盆地 ; Tarim Basin
• 页码：p.714-727
• 图表：8 illus., 25 refs.
• 分类号：0300
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

The view that geotectonics was controlled by deep dynamic action of the earth has long been accepted, because the compression between Tarim Plate, Sino-Korea Plate and Mongolia Plate resulted in the formation of the Beishan orogenic belt, which has been evidenced by a comprehensive analysis of regional tectonics in Beishan Mountain and its adjacent areas. The authors analyzed the distribution of ore deposits in Beishan area and found that many large ore deposits occur on the northern side of the acid batholith and are closely associated with northward dipping thrust faults and stocks. The acid batholith related to mineralization also has northward dipping characteristics, and hence the ore-forming magma could be emplaced on the northern side of the batholith. These ore-forming features provide important means and clues to the prospecting work in similar areas.