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《Earth Science Frontiers》 2007-03
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Tertiary Duofuton Na-rich mafic volcanic rocks,on northeastern margin of the Qinghai-Tibet Plateau and their tectonic implications

Guo Anlin1, Zhang Guowei1, Sun Yangui1,2, Cheng Shunyou11.State Key Laboratory of Continental Dynamics/Department of Geology,Northwest University,Xi'an 710069,China2.Qinghai Institute of Geological Survey, Xining 810012, China  
The Tertiary Duofuton volcanic rocks, located on the northeastern margin of the Qinghai-Tibet Plateau, belong to a Na-rich mafic volcanic system. The rocks are characterized by the(La/Yb)N ratios of 6-11, average ΣREE of 117, general enrichment in incompatible elements, Pb depletion and weak Nb and Ta positive anomalies. Their Nb/U and Ce/Pb ratios are 30 and 17 on average, respectively. The 87Sr/86Sr ratios are 0.704 1-0.706 9, 143Nd/144Nd=0.512 9(εNd(t)=6), and Δ207Pb/204Pb and Δ208Pb/204Pb =11-19 and 73-84, respectively. Coupled with high 87Sr/86Sr ratios, they show Dupal anomalies. Generally, these mafic rocks are OIB-like intracontinental volcanics and the source region exhibits a mixture between DM and EMⅡ, some of the rocks are obviously contaminated by crustal materials. The complexity of OIB for these mafic volcanic rocks may have been inherited from the proto-and paleo-Tethyan mantle in the region and hence it is in-situ and original in nature, and possibly not related to the eastward extrusion of materials from the Qinghai-Tibet Plateau. In comparison with coeval volcanics in adjacent areas, it can be inferred that the mantle region in the northeastern margin is heterogeneous on a small scale. The development of the Cenozoic volcanics could have been triggered by the N-S trending tectonics.
【Fund】: 国家自然科学基金资助项目(40572138 40234041)
【CateGory Index】: P588.1
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Chinese Journal Full-text Database 10 Hits
1 ZHENG Hong-bo~ 1,2 BUTCHER Katherine~3 POWELL Chris~3 1 ( Laboratory of Marine Geology, Tongji University, Shanghai 200092) 2 (Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054) 3 (Tectonic Special Research Centre, The Un;Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau --I Stratigraphy and Petrology[J];Acta Sedimentologica Sinica;2002-02
2 ZHENG Hong-bo 1,2 BUTCHER Katherine3 POWELL Chris3 1(Laboratory of Marine Geology, Tongji University, Shanghai 200092) 2(Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054) 3(Tectonic Special Research Centre, The University of Western Australia, Perth);Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——Ⅱ Facies Analysis[J];Acta Sedimentologica Sinica;2003-01
3 ZHANG Guo-wei,DONG Yun-peng,YAO An-ping (Department of Geology,Northwest University,Xi'an710069,China);Some thoughts on the study of continental dynamics and orogenic belts[J];Chinese Geology;2002-01
4 LI Yong 1 ,HOU Zhong-jian 1 ,SI Guang-ying 1 ,A.L.DENSMORE 2 ,ZHOU Rong-jun 3 ,M.A.ELLIS 4 ,LI Yong-zhao 1 ,LIANG Xing-zhong 1(1.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu610059;Cenozoic tectonic sequence and tectonic events at the eastern margin of the Qinghai-Tibet plateau[J];Chinese Geology;2002-01
5 ChEN Hong-wei1, LUO Zhao-hua2,3, MO Xuan-xue2,3, LIU Cheng-dong4, KE Shan2(1. Key Laboratory of Water Resources and Environment Engineering, Beijing, China University of Geosciences, Beijing 100083, China;2.School of Earth Sciences & Resources, China University of Geosciences, Beijing 100083, China3. Key Laboratory of Lithospheric Structure, Deep Processes and Exploration Techniques, Ministry of Education, Beijing 100083, China;4. East China Institute of Technology, Fuzhou 344000, Jiangxi China);Underplating mechanism of Triassic granite of magma mixing origin in the East Kunlun orogenic belt[J];Chinese Geology;2005-03
6 Niu Zhijun\+\{1)\}, Ma Zongjin\+\{2)\}, Chen Xinlian\+\{3)\}, Zhang Zusheng\+\{4)\}, Wang Qi\+\{5)\},You Xinzhao\+\{5)\} and Sun Jianzhong\+\{1)\}\;1) Department of Monitoring and Prediction, CSB, Beijing\ 100036 2) Institute of Geology, CSB, Beijing;CRUSTAL MOVEMENT OBSERVATION NETWORK OF CHINA[J];Crustal Deformation and Earthquake;2002-03
7 Zhu Bingquan Zhang Yuquan Xie Yinwen(Institute of Geochemistry, Academta Sinica, Guangzhou 510640);Nd, Sr AND Pb ISOTOPIC CHARACTERISTICS OF CENOZOIC ULTRA-POTASSIC VOLCANIC ROCKS FROM EASTERN ERHAI, YUNNAN AND THEIR IMPLICATIONS FOR SUBCONTINENT-MANTLE EVOLUTION IN SOUTHWESTERN CHINA[J];Geochimica;1992-03
8 WAN Yusheng1,2, LUO Zhaohua3, LI Li31. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; 2. Beijing SHRIMP Lab, Beijing 100037, China;3. China University of Geosciences, Beijing 100083, China;3.8 Ma: SHRIMP U-Pb zircon dating of the younger alkali basaltin the Qinghai-Xizang Plateau[J];Geochimica;2004-05
9 Wu Gongjian Xiao Xuchang Li Tingdong (Chinese Academy of Geological Sciences,Beijing 100037);EXPOSE THE UPLIFT OF QINGHAI-TIBET PLATEAU: YADONG-GOLMUD GEOSCIENCE TRANSECT IN QINGHAI-TIBET PLATEAU,CHINA[J];EARTH SCIENCE;1996-01
10 MU ZHI-GUO TONG WEI(Department of Geology, Peking University, Beijing, China)GARNISS H. CURTIS(Department of Geology & Geophysics, University of California, Berkeley, CA 94720, U. 5. A.);TIMES OF VOLCANIC ACTIVITY AND ORIGIN OF MAGMA IN TENGCHONG GEOTHERMAL AREA,WEST YUNNAN PROVINCE[J];Chinese Journal of Geophysics;1987-03
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