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《》 2006-01
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Interaction between Crust and Weakening Lithospheric Mantle: Taking the Yanshan Orogenic Belt as an Example

LU Feng-xiang, ZHENG Jian-ping, ZHANG Ruksheng, SHAO Ji-an, LI Wu-ping, YU Chun-mei Faculty of Earth Sciences, China University of Geosciences , Wuhan 430074, China School of Earth and Space Science , Peking University, Beijing 100871, China School of Civil Engineering, Guangzhou University, Guangzhou 510405, China  
Four-period calc-alkaline volcanic rocks are widespread in the Yanshan erogenic belt. The components of magma sources were controlled predominantly by the interaction between the continental crust and upper mantle near MOHO surface. The Tiaojishan and Yixian formations are the representative types of volcanic activity. The petrological features of Tiaojishan Formation volcanic rocks are relatively uniform, geochemical parameters varies at a narrow range and the AFC processes of magma are not strong enough, which indicates that the components of the magma source were not very complex. The estimated thickness of the crust was 40 - 45 km during the Early to Middle Jurassic. We infer that Tiaojishan tra-chyandesite magma was melted from amphibole-bearing garnet granulite + underplating basalts at thickening crust condition. A possible model, delaminating lower continental crust into the underlying weakening lithospheric mantle and interaction between them, has been proposed as one means to explain the genesis of basic-middle basic magma in the Yixian Formation. The inferred source of these magmas was lower crust + weakening lithosphere. Rheological behavior of the lithospheric mantle has been heterogeneously translated from rigid to ductile. This translation process was induced by the effects of fluid, melt, water released from mantle minerals, shear stress and increasing temperature in the lithospheric mantle beneath the small extension basin and above the uplifted asthenospheric diapir after approximately 135 Ma These local areas were the preferable sets to hold the delaminated lower crust. The interaction between the foundering continental lower crust and the underlying weakening lithospheric mantle may be compared with the interaction between the subducting ocean crust and mantle wedge at a subduction zone
【Fund】: 教育部博士点基金项目(No.20010491010) 国土资源部基础研究专项计划(No.20001010203) 国家自然科学基金项目(No.40372103)
【CateGory Index】: P542.2
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Chinese Journal Full-text Database 10 Hits
1 Wu Fuyuan,Sun Deyou (Changchun University of Science and Technology,Changchun 130026);THE MESOZOIC MAGMATISM AND LITHOSPHERIC THINNING IN EASTERN CHINA[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;1999-04
2 XU Wen_liang, WANG Dong_yan,WANG Si_min (Changchun University of Science and Technology, Changchun 130026, China);pTtc MODEL OF MESOZOIC AND CENOZOIC VOLCANISMS AND LITHOSPHERIC EVOLUTION IN EASTERN CHINA[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;2000-04
3 Wang Dongpo Zhang Liping L.A.Frakes Liu Li Ji Guixia Gao Fuhong (Changchun Univ. of Earth Sci., 130026)(Univ. of Adelaid, South Australia, 5001);THE DISCOVERY AND SIGNIFICANCE OF CRETACEOUS ICERAFTING DEPOSITS IN SONGLIAO BASIN[J];;1996-04
4 Liu Shengcheng (Research Center for Basin and Reservoir,University of Petroleum,Beijing, 102200);Stratigraphic research on the lower member of the Devonian Wuzhishan Formation of Nayi,Guangxi[J];JOURNAL OF STRATIGRAPHY;1997-03
5 Wang Dongfang Zhou Shiguang Sun Chenglin (Shenyang Institute of Geology and Mineral Resources);REE DETERMINATION AND REE DISTRIBUTION PATTERNS OF MESO-CENOZO1C VOLCANIC ROCKS IN CENTRAL-WESTERN LIAONING PROVINCE AND THEIR GEOTECTON1C IMPLICATIONS[J];Geochimica;1985-02
6 ZHOU Xin- hua1, ZHANG Guo- hui1, YANG Jing- hui1, CHEN Wen- ji 2, SUN Min3 (1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Institute of Geology, China Seismological Bureau, Beijing 100029, China; 3. Depart;Sr-Nd-Pb isotope mapping of Late Mesozoic volcanic rocks across northern margin of North China Craton and implications to geodynamic processes[J];Geochimica;2001-01
7 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
8 LI Xian hua, LIU Ying, TU Xiang lin, HU Guang qian, ZENG Wen(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Precise determination of chemical compositions in silicate rocks using ICP AESand ICP MS: A comparative study of sample digestion techniquesof alkali fusion and acid dissolution[J];Geochimica;2002-03
9 WEI Gang jian, LIANG Xi rong, LI Xian hua, LIU Ying(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Precise measurement of Sr isotopic composition of liquid and solid base using (LP)MC ICPMS[J];Geochimica;2002-03
10 LIANG Xi rong, WEI Gang jian, LI Xian hua, LIU Ying(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Precise measurement of ~(143)Nd/~(144)Nd and Sm/Nd ratios using multiple collectors inductively coupled plasma mass spectrometer (MC ICPMS)[J];Geochimica;2003-01
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