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《Earth Science Frontiers》 2004-03
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Processes and mechanism of Mesozoic lithospheric thinningin eastern North China Craton: Evidence from Mesozoicigneous rocks and deep-seated xenoliths

XU Wen-liang~1, WANG Qing-hai~1, WANG Dong-yan~1, PEI Fu-ping~1, GAO Shan~2(1. College of Earth Sciences, Jilin University, Changchun 130061, China;2. College of Earth Sciences, China University of Geosciences, Wuhan 430074, China)  
Mesozoic magmatisms in the eastern North China Craton (NCC) can be subdivided into four periods on the basis of the last isotopic geochronological data, i.e., the late Triassic (205~225 Ma) alkaline magmatism, the middle-late Jurassic (155~160 Ma) granitic magmatism, the early Cretaceous (112~132 Ma) bi-modal magmatism, and the late Cretaceous (73~92 Ma) alkaline basaltic magmatism. The discovery of eclogite xenoliths and their geochronological data (220 Ma±) in Mesozoic intrusive in the Xu-Huai region imply that the thickening of continental crust happened in the eastern North China craton in the Early Mesozoic. The break-off of subducted slab, quick exhumation of high- and ultrahigh-pressure metamorphic (UHPM) rocks, and the late Triassic (205~225 Ma) alkaline magmatism suggest the beginning of Mesozoic lithospheric thinning in the NCC. The delamination could be a major mechanism to result in the thinning of lithospheric mantle in the Early Mesozoic. The middle-late Jurassic (155~160 Ma) granitic magmatism formed in post-orogenic extensional environment, implying the continuity and development of Mesozoic lithospheric thinning. The early Cretaceous (112~132 Ma) bi-modal magmatism implys the coming of the peak period of Mesozoic lithospheric thinning. The silica-rich melt metasomatism in the mantle-derived dunite xenoliths and high~(87)Sr/~(86)Sr ratios and low ε(Nd,t) values of basalts indicate that the chemical erosion of the asthenosphere to the lithospheric mantle could be a major mechanism to result in the thinning of lithospheric mantle in the period. The late Cretaceous (73~92 Ma) alkaline basaltic magmatism and the existence of “oceanic-like” mantle xenoliths indicate the decreasing of isothermal plane and the accretion of lithospheric mantle.
【Fund】: 国家自然科学基金资助项目 (4 0 1 72 0 30 ;40 1 330 2 0 ) ;; 高校博士学科点基金资助项目 (2 0 0 1 0 1 830 0 7)
【CateGory Index】: P588.1
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3 WU FuYuan,XU YiGang,GAO Shan and ZHENG JianPing 1.State Key Laboratory of Lithoshperic Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Key Laboratory of Isotopic Geochronology and Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences, Guangzhou 510640,China 3.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China;Lithospheric thinning and destruction of the North China Craton.[A];[C];2009
4 CHEN ZhiGuang,ZHANG LianChang,WU HuaYing,WAN Bo and ZENG QingDong 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100039,China;Geochemistry study and tectonic background of A style host granite in Nianzigou molybdenum deposit in Xilamulun molybdenum metallogenic belt,Inner Mongolia.[A];[C];2009
5 GUO ZhengFu,LIU JiaQi,CHEN XiaoYu and LI XiaoHui Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Effect of volatiles erupted from Mesozoic activities in Yanliao area of North China on paleo-environmental changes.[A];[C];2009
6 ZHANG Qi,WANG Yuan-long,JIN Wei-jun,LI Cheng-dong 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China;Eastern China Plateau during the Late Mesozoic:evidence,problems and implication.[A];[C];2009
7 ZHANG Qi Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;“Blue storm”and“Red revolution”:On developing new continent tectonics theory[A];[C];2009
8 ZHANG Qi,PAN GuoQiang,LI ChengDong,JIN WeiJun and JIA XiuQin 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Department of Earth Sciences,Nanjing University,Nanjing 210093,China 3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China 4.Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100039,China;Problems of granites:some crucial questions on granite study(5).[A];[C];2009
9 ZHANG Qi,PAN GuoQiang,LI ChengDong,JIN WeiJun and JIA XiuQin 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Department of Earth Sciences,Nanjing University,Nanjing 210093,China 3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China 4.Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100039,China;Study of granite in the 21~(st) century:where we go? some crucial questions on granite study(6).[A];[C];2009
10 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China);Adakite research:retrospect and prospect[A];[C];2009
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8 LIN Jing_qian 1, TAN Dong_juan 1, LI Jian_hua 2, LIU Zhan_sheng 1 (1.Changchun University of Science and Technology, Changchun 130026, China; 2.Jiangsu Mineral Exploration and Development Co, Nanjing 210018, China);EARLY JURASSIC BANJING INTRUSIVE COMPLEX OF SOUTHERN MARGINAL ZONE OF NORTH CHINA BLOCK,XUZHOU[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;2000-03
9 LIN Qiang 1, GE Wen_chun 1, SUN De_you 1, WU Fu_yuan 1, WON Chong_kwan 2, LEE Moon_won 2, YUN Sung_hyo 3, JIN Myung_shik 4, MIN Kyung_duck 5,KWON Chi_soon 6 (1.Changchun University of Science and Technology,Changchun, 130026; 2.Kang Won Nation;GENETIC RELATIONSHIPS BETWEEN TWO TYPES OF MESOZOIC RHYOLITE AND BASALTS IN GREAT XING’AN RIDGE[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;2000-04
10 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
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