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《Journal of Jilin University(Earth Science Edition)》 2012-02
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Crustal Radiogenic Heat and Mantle Geothermal Status in Tibetan Plateau Based on P-Wave Velocity

Guan Yan-wu1,Guan Ye2,Gao Rui2,Sun Xiao-hua3,Jin Xu1 1.College of GeoExploration Science and Technology,Jilin University,Changchun 130026,China 2.Lithosphere Research Center,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037 3.Economics School,Jilin University of Finance and Economics,Changchun 130017,China  
A large amount of geophysical data of Tibetan Plateau has been accumulated since 1974 when the modern geophysical exploration about Tibetan Plateau began.P-wave velocities of 23 deep seismic sounding profiles are collected and relationship curve of crustal radiogenic heat and P-wave velocity(A-Vp) in each profile was plotted.The mantle heat flow contour map of Tibetan Plateau is drawn reference to terrestrial heat flow data sets.There is a very high mantle heat flow area on the Bangong-Nujiang suture zone,Indus-Yarlung suture and Lhasa block.It can be infered that the magma under the area is possible active.
【Fund】: 国家自然科学基金项目(40974047);; 中国地质科学院地质研究所基本科研业务费(2010-sys-04);; 国土资源部专项(SinoProbe-09-01);; 吉林大学基本科研业务费(450060445194)
【CateGory Index】: P631.4
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