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《Geotectonica Et Metallogenia》 2005-03
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A NUMERICAL MODELING STUDY ON THE “ASTHENOSPHERE UPWELLING” OF SOUTH CHINA SEA

CUI Xuejun 1, XIA Bin 1, ZHANG Y H 2, LIU Baoming 1 , WANG Ran 1 and YAN Yi 1 (1. CAS Key Laboratory of Marginal Sea Geology and Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. CSIRO Exploration & Mining, P.O.Box 1130, Bentley, WA 6102, Australia)  
A numerical approach was used to explore the following key issues: how does the “asthenosphere upwelling” behave in terms of mechanism towards the expansion of the South China Sea? and how to evaluate such a behavior? Our results indicate that asthenosphere upwelling is much more efficient for the lithospheric thinning in the upper mantle but is still inefficient for crust thinning. It is the combination of mechanical extension and asthenosphere upwelling that proves to be the most efficient way to thin the entire lithosphere, and that represents the most likely driving force for the opening and spreading of the South China Sea.
【Fund】: 中国科学院知识创新工程重要方向性项目(KZCX2-SW-117)资助.
【CateGory Index】: P542.5;P736.12
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【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Zhu Jieshou;THE CHARACTERISTICS OF SUBPLATE DIVISION OF CRUST AND UPPER MANTLE IN THE CONTINENT OF CHINA[J];;1986-01
2 ZOU Heping (Changsha Institute of Geotectonics, A cademia Sinica, Changsha, 410013);ON THE PROBLEM ABOUT THE CRUST'S ATTRIBUTION OF SOUTH CHINA SEA BASIN——DISCUSSION FROM COMPARATIVE STUDY ON BASALTS OF SEAMOUNTS IN SOUTH CHINA SEA BASIN AND THE NEIGHBORING AREAS[J];Geotectonica Et Metallogenia;1993-04
3 CHEN Guoda(Changsha Institute of Geotectonics, Academia Sinica; International Research Center forGeodepressional (Diwa ) Tectonics and Metallogeny; WG4, Tectono - Magmatic Activization(Diwa ), IAGOD/CTOD, Changsha 410013, China );THE MARGINAL EXTENSIONAL BELT OF EAST ASIA CONTINENT INVESTIGATING THE ORIGINOF A DISCRETE CONTINENTAL MARGIN[J];GEOTECTONICA ET METALLOGENIA;1997-04
4 XIA Bin~1, CUI Xuejun~(1,2), XIE Jianhua~1 and WANG Ran~1 (1. Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry & South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510640, China;2. Jiangxi Bureau of Geological Survey, Nanchang, JX 330002, China);THINKING ABOUT THE DYNAMICS MECHANISM STUDY ON FORMATION AND EVOLUTION OF SOUTH CHINA SEA[J];Geotectonica Et Metallogenia;2004-03
5 Wang Xianjue Wu Mingqing (Institute of Geochemistry, Academia Sinica)Liang Dehua Yin Aiwu (South China Sea Institute of Oceanography, Academia Sinica);SOME GEOCHEMICAL CHARACTERISTICS OF BASALTS IN THE SOUTH CHINA SEA[J];Geochimica;1984-04
6 Chen Daogong Pen Zicheng (Department of Earth and Space Science, University of Science and Technology of China);K-Ar AGES AND Pb, Sr ISOTOPIC CHARACTERISTICS OF CENOZOIC VOLCANIC ROCKS IN SHANDONG, CHINA[J];Geochimica;1985-04
7 Zhu Bingquan Wang Huifen Yang Xucchang(Institute of Geochemistry, Academia Sinica);GEOCHRONOLOGY OF CENOZOIC VOLCANISM IN EAST CHINA AND GLOBAL CHANGES OF TECTONIC ENVIRONMENT[J];Geochimica;1988-03
8 Liu Beiling Chen Yuwei Zhu Bingquan(Institute of Geochemistry, Academia Sinica);ORIGIN OF CENOZOIC BASALTS FROM JINBOHU, NORTHEAST CHINA AND CHEMICAL CHARACTERISTICS OF THEIR MANTLE SOURCE——Sr-Pb ISOTOPE AND TRACE ELEMENT EVIDENCE[J];Geochimica;1989-01
9 Zhu Bingquan Wang Huifen(Institute of Geochemistry, Academia Sinica);Nd-Sr-Pb ISOTOPIC AND CHEMICAL EVIDENCE FOR THE VOLCANISM WITH MORB-OIB SOURCE CHARACTERISTICS IN THE LEIQIONG AREA, CHINA[J];Geochimica;1989-03
10 WANG Qiang,ZHAO Zhen-hua,XIONG Xia o-lin,XU Ji-feng (Guangzhou Institute of Geochemistr y,Chinese Academy of Sciences,Guangzhou510640,China);Melting of the underplated basaltic lower crust:Evidence from the Shaxi adakitic sodic quartz diorite-porphyrites,Anhui Province,China[J];Geochimica;2001-04
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