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《Journal of Jiling University (Earth Science Edition)》 2004-04
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The constitution and importance geological events of Pre-Devonian in the Dulan, Qinghai

HAO Guo-jie~(1,2 ),LU Song-nian~(2),XIN Hou-tian~(2),WANG Hui-chu~(2) (1.College of Earth Science, Jilin University, Changchun130061,China;2.Tianjin Institute of Geology and Mineral Resources, Tianjin300170,China)  
Research on geology, geochemistry and geochronology of the old, Pre-Devonian continent in the Dulan area, Qinghai indicates that the continent can be divided into three tectonic units, namely, the Olongbuluck old continent block, the Shaliuhe UHP collision belt and the Caidam continent block. The Olongbuluck old continent block consists mainly of the Delingha Gneiss, Mohe gneiss, Dakandaban Group, Wandonggou Group and Quanji Group. The Shaliuhe UHP collision belt is composed mainly of the Shaliuhe Group, granodiorite gneiss, tonalite gneisss, moyite gneiss, eclogite, Tanjianshan Group and ophiolite. The Caidam old continent block is made up of the paleo-Proterozoic Jinshuikou Group and sill-cord-granitic gneiss. Some important geological events in Pre-Devonian, especially those related to the assembly and break-up of the Rodinia supercontinent have been defined in detail. Meanwhile, the geological age of these important events and sequence had been confirmed by advanced isotopic geochronology method. These events have provided evidences for studying the relation and location of Rodinia assembly and its break-up in Meso- and Neo- Proterozoic in China and for international correlation.
【Fund】: 国家自然科学基金重点项目(40032010-C);; 中国地质调查局基础调查项目(20011300062);(200013000153)
【CateGory Index】: P534
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