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《Acta Geologica Sinica》 2005-01
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Characteristic and Distribution of the Partial Melting Layers in the Upper Crust: Evidence from Active Hydrothermal Fluid in the South Tibet

LI Zhenqing, HOU Zengqian, NIE Fengjun, MENG Xiangjin Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037  
During the process for carrying out of a series of geophysical probe, a suit of were observed along the Yadong—Gulou rift valley zone. Combining with data from other geophysical sections, a low velocity-high conductivity layer was recognized in the upper crust in the southern Tibet. These seismic bright spots do lie in the low velocity-high conductivity layer. For these bright spots and the low velocity-high conductivity layer, there are still two kinds of understandings and opinions: one is saliferous supercritical fluid; the other is partial melting layer of the upper crust. Due to lack of effective means and methods, their characteristic and distribution were still guessed. Based on the research on the violent hydrothermal activity of the south Tibet, this paper made an attempt to discuss the characteristic of these bright spots and low velocity-high conductivity layer from other point. The research on helium isotope composition of hot spring's gas, geochemical characteristic of spring water, and former modeling for temperature field suggest that the low velocity-high conductivity layer was composed of rather silicate magma than water fluid. Theses research provide new evidences for exist of the partial melting layers. What's more, this paper discusses how the partial melting layer driving the active hydrothermal system to circulate and flow, At last, and restrict the spatial distribution of the partial melting layer based on the distribution of hot springs and temperature field.
【Fund】: 国家重点基础研究规划 973项目 (编号 2 0 0 2 CB412 60 6);; 国家自然科学基金项目 (编号 40 3 0 2 0 2 8)资助的成果
【CateGory Index】: P542
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2 GUO ZhengFu;ZHANG MaoLiang;CHENG ZhiHui;ZHANG LiHong;LIU JiaQi;Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences;;Fluxes and genesis of greenliouse gases emissions from typical volcanic fields in China[A];[C];2015
3 JIANG Di-Di;JIANG Wei-Wei;XU Yi;HAO Tian-Yao;HU Wei-Jian;YU Jing-Feng;Institute of Geology and Geophysics,Chinese Academy of Sciences,Key Laboratory of Petroleum Resources Research,Chinese Academy of Sciences;University of Chinese Academy of Sciences;;Characteristicsof crustal structure and their relation with major earthquakes in western China[A];[C];2015
4 CHEN Zheng;YUN Fei;XIAO Wei; LIU Da-wen; YUAN Chun-hua;HAN Jiu-xi;Development and Research Center of China Geological Survey;Institute of Mineral Resources,CAGS;Infomation Center of Ministry of Land and Resources;;New Advances on Metallogenic Studies and Mineral Exploration of Three Ore Deposits occurring in the Southern Mongolia[A];[C];2010
5 TANG Ju-xing;Dorji;LIU Hong-fei;LANG Xing-hai;ZHANG Jin-shu;ZHENG Wen-bao;YING Li-juan;MLR Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;Geology & Mineral Exploration Development Bureau of Tibet Autonomous Region;Geoscience institute, Chengdu University of Technology;;Minerogenetic Series of Ore Deposits in the East Part of the Gangdise Metallogenic Belt[A];[C];2012
6 WANG Yi-yun;TANG Ju-xing;ZHENG Wen-bao;LIN Bin;LENG Qiu-feng;CHEN Wei;DING Shuai;SONG Jun-long;XU Yun-feng;Chengdu University of Technology;MLR Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;;A Tentative Discussion on Ore Fabric and Genesis of the Zhaxikang Zn-polymetallic Deposit, Lhunze County, Tibet[A];[C];2012
7 LIU Cheng-lin;MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences;;Characteristics and Formation of Potash Deposits in Continental Rift Basins:A Review[A];[C];2013
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