• 责任者：Zhao Zhenming (Xi’an Institute of geology and Mineral Resources ; Xi’an ; 710054) ; Ma Huadong
• 刊名：Geological Review
• 出版年：2008
• 卷期：54(1)
• 关键词：闪长岩 ; diorites ; 花岗岩 ; granite ; 昆仑山 ; Kunlun Mountains
• 页码：p.47-56
• 图表：7 illus., 2 tables, 37 refs.
• 分类号：0801
• issnNo：ISSN0371-5736
• isbnNo：CN11-1952/P

The Early Devonian intrusive rocks in central Kunlun fault and its adjacence area in east Kunlun is effected by central Kunlun fault activity,  deformed strong,  showed irregularly lens- shaped in horizontal plane,  distributed approximately west—east direction along the central Kunlun fault. Based on regional geological data and tectonic setting diagrams of granites,  the Early Devonian intrusive rocks studied in this paper are post- collision-orogenic granites,  the material resources originated from interaction of crust—mantle.   It is concluded that the collision-orogenic movement had taken place in east Kunlun during late Caledonian orogeny.