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《Chinese Geology》 2005-04
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Geochemical characteristics and zircon U-Pb ages of island-arc basic igneous complexes in the Tianshui area,West Qinling

PEI Xian-zhi1,LI Zuo-chen1,DING Sa-ping1,2,LI Yong1,HU Bo1,LIU Hui-bin1(1.Faculty of Earth Sciences and Land Resources,Chang'an University,Xi'an 710054,Shaanxi,China;2.Gansu Institute of Geological Survey,Lanzhou 730000,Gansu,China)  
The Liushuigou intermediate-basic meta-igneous complex at Guanzizhen,Tianshui,is composed mainly of metagabbro-metagabbro diorite-metadiorite,and the Baihua basic meta-igneous complex consists mainly of pyroxenite-gabbro (-diorite)-diorite-quartz diorite.They form a relatively complete comagmatic evolutionary series.The geochemical characteristics of basic to intermediate-basic igneous rocks indicate that they belong to a tholeiite suite.Their chondrite-normalized REE patterns are of nearly flat and slightly LREE-enriched type,and their primitive mantle-normalized and MORB-normalized trace element spidergrams are generally similar;the LILEs Cs,Ba,Sr,Th and U are enriched,while Rb and K and the HFSEs Nb,P,Zr,Sm,Ti and Y are depleted.All these show comagmatic evolutionary and genetic characteristics.The tectonic environment discrimination by trace elements reveals that these igneous complexes formed in an island-arc setting.The TIMS single-zircon U-Pb age for the Liushuigou intermediate-basic meta-igneous rocks in the Guanzizhen area is 507.5±3.0 Ma,representing the age of these igneous complexes,which indicates that island-arc-type magmatic rocks in the north zone of the West Qinling are Late Cambrian in age and also reveals that the timing of subduction of the paleo-ocean basin represented by the Guanzizhen ophiolite and resulting island-arc-type magmatic activity is probably Late Cambrian to Early Ordovician.
【Fund】： 国家自然科学基金项目(40234041 40572121);; 教育部科学技术研究重点项目(104175);; 中国地质调查局地质大调查项目(200013000154)资助
【CateGory Index】： P588.1;P597.3
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7 Zhou Dingwu Zhang Chengli Liu Liang Wang Juli Liu Yinyu (Department of Geology,Northwest Uniuersity,Xi'an) Zhang Zongqing (Institute of Geology,CAGS,Beijing);Sm Nd Dating of Basic Dykes from Wudang Block and a Discussion of Related_Questons[J];;1998-01
8 Yang Zhihua(Xi'an Engineering College, Xi'an, 710054)Zhang Chuanlin Zhu Lihua(Department of Earth Sciences, Nanjing University, Nanjing, 210093)Deng Yating(The Information Centre, Shaanxi Bureau of Geology and Mineral Resources, Changan, 710100);THE TYPE AND STAGE OF BASIN MOUNTAIN TRANSFORMATION IN CONTINENTAL OROGEN--TAKING QINLING AS AN EXAMPLE[J];EARTH SCIENCE FRONTIERS;1999-04
9 YANG Zhi\|hua 1, SU Sheng\|rui 1, LI Yong 1, ZHANG Chuan\|lin 2, ZHOU Mei\|fu 3, ZHAO Tai\|ping 4 (1 Chang’an University, Xi’an 710054, China; 2 Nanjing Institute of Geology and Mineral Resources, Ministry of Land and Resources, Nanjin;DISCUSSION ON SOME KEY PROBLEMS ABOUT THE GEOTECTONICS OF CHINA[J];Earth Science Frontiers;2001-02
10 Wang Hongzhen(China University of Geosciences, Beijing, 100083);SPECULATIONS ON EARTH′S RHYTHMS AND CONTINENTAL DYNAMICS[J];EARTH SCIENCE FRONTIERS;1997-Z2
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