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柴达木盆地北缘盆山耦合作用特征及砂岩型铀成矿远景分析
引用本文:王夏涛,付成铭,李海森.柴达木盆地北缘盆山耦合作用特征及砂岩型铀成矿远景分析[J].矿产与地质,2008,22(6):492-495.
作者姓名:王夏涛  付成铭  李海森
作者单位:河南省有色金属地质矿产局第五地质大队,郑州,450016
摘    要:柴北缘盆地-造山带体系在西北地区有一定的代表性,盆山耦合过程与成矿的研究是当代地质科学研究的热点之一。以盆山耦合体系演化、铀矿化目的层改造作用、砂岩型铀成矿理论为基础,将柴北缘划分四大构造单元,讨论了主要构造运动时期的盆山耦合特征,分析了盆山耦合体系对休罗系、第三系的改造作用,指出了该区的主要找矿类型。

关 键 词:砂岩型铀矿类型  盆山耦合  改造作用  柴达木盆地北缘

Basin-mountain coupling characters of northern edge of Qaidam Basin and the prospect area for sandstone-host U deposit
WANG Xia-tao,FU Cheng-ming,LI Hai-sen.Basin-mountain coupling characters of northern edge of Qaidam Basin and the prospect area for sandstone-host U deposit[J].Mineral Resources and Geology,2008,22(6):492-495.
Authors:WANG Xia-tao  FU Cheng-ming  LI Hai-sen
Institution:WANG Xia-tao, FU Cheng-ming, LI Hal-sen (No. 5 Geological Brigade of Henan Non-ferrous Metals Geology and Mineral Resources Bureau, Zhengzhou 450016, China)
Abstract:The system of basin-orogenic belt on northern edge of Qaidam Basin is representative in Northwest China. The relationship between basin-mountain coupling process and metallogeny is a hot spot in modern geological research. Based on the evolvement of basin-mountain coupling, alteration on target bed for U mineralization, and metallogenic theory of sandstone-host U deposit, the study has plotted the north edge of Qaidam Basin into four major tectonic units, discussed the characteristics of basin-mountain coupling during the major period for tectonic movements, analyzed the alteration on Jurassic and Tertiary strata by basin- mountain coupling system, and pointed out the major prospecting types in this area.
Keywords:sandstone-host U deposit  basin-mountain coupling  alteration  northern edge of Qaidam Basin
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