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《Geotectonica Et Metallogenia》 2009-03
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Adakites or Adakitic Rocks and Associated Metallogenesis in Eastern China

LI Yin1,2,LING Mingxing1,2,DING Xing1,2,LIU Jian1,2,HAN Feng1,2 and SUN Weidong1(1.Guangzhou Institute of Geochemistry,Chinese Academic of Sciences,Guangzhou 510640,Guangzhou,China;2.Graduate University of Chinese Academic of Sciences,Beijing 100049,China)  
Adakites were proposed over a decade ago to be products of the melting of young subducted oceanic crust,belonging to the intermediate-acid volcanic and intrusive rock,which have distinct characteristics of high Al2O3,Sr contents and Sr /Y ratios,but low Y,Yb contents and K2O/Na2O ratios,without obvious Eu anomalies. Since discovered and named 30 years ago,adakite is universally acknowledged as one of the frontier topics in earth science. There are two main reasons why the study on adakites is not forwarding rapidly. One is their special geochemical nature,the other is metallogenesis. Eastern China is the most abundant adakites concentrated area,mostly distributed in the Lower Yangtze Region and Eastern Shandong and Shanxi-Beijing-Liaoning (subdivided into Beijing-Hebei and northeast region) three districts. Among them except Beijing-Hebei,other three regions are all important copper-gold metallogenic belts. Four genetic model proposed before by other geologists are as follows: ancient thickening lower continental crust melting,underplated basaltic lower crust melting,melting of delaminated lower continental crust and mid-ocean ridge subduction. However,the relationship between copper-gold metallogenesis and adakites is still controversial. Generally,adakitic magmas are thought to be enriched in fluid,with high oxygen fugacity and mafic source rock,which are favored by Cu,Au and other deeply-source metals to be extracted,enriched,and finally mineralized.
【CateGory Index】: P594
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10 Zhang Qi1 Jiao Shoutao2 Wu Haoruo1 Jin Weijun1 Li Chengdong3 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029 2 School of Earth Sciences and Natural Resources, China University of Geosciences(Beijing),Beijing 100083 3 Tianjin Institute of Geology and Mineral Resources,China Geological Survey, Tianjin 300170;Palaeotopographic map of the Triassic of China[J];Journal of Palaeogeography;2013-02
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1 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Collision and granite:Collision is a tectonic event,not a tectonic environment[A];[C];2013
2 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);DISCUSS ON THE RELATIONSHIP BETWEEN GRANITIC ROCKS AND Au-Cu-W-Sn-MINERALIZATION[A];[C];2014
3 Zhang Qi~1 Jiao Shoutao~2 Wu Haoruo~1 Jin Weijun~1 Li Chengdong~3 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029 2 School of Earth Sciences and Natural Resources,China University of Geosciences(Beijing),Beijing 100083 3 Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170;Palaeotopographic map of the Triassic of China[A];[C];2014
4 Qingdong Zeng~*,Jianming Liu,Kezhang Qin,Hongrui Fan,Shaoxiong Chu,Yongbin Wang and Lingli Zhou Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Types,characteristics,and time-space distribution of molybdenum deposits in China[A];[C];2014
5 ZHANG Qi;Institute of Geology and Geophysics,Chinese Academy of Sciences;;Geodynamic implications of continental granites[A];[C];2015
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4 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
5 ZHANG Jiongfei1, 2,ZHU Qun1, 2,SHAO Jun2, 3,JIN Chengzhu2 (1.Institute of Resources and Civil Engineering, Northeast University, Shenyang 110004,China;2.Shenyang Institute of Geology and Mineral Resources, Shenyang110033,China;3.College of Earth Sciences, Jilin University, Changchun130026, China);UPb AGE OF MONOMINERAL ZIRCON OF BADAOKA QUARTZ-DIORITE IN INNER MONGOLIA AND ITS SIGNIFICANCE[J];Journal of Changchun University of Science and Technology;2003-04
6 Qu Yixiu;Liu Zhiguo(Qinhuangdao college, Northeast Uni.,Qinhhuangdao 066000);GENETIC RELATION BETWEEN YANSHANIAN GRANITES AND GOLD MINERALIZATION,IN EASTERN HEBEI[J];;1995-04
7 WU Guang1,2, LI Zhongquan3, LI Zhitong2(1.College of Earth Sciences, Jilin University, Changchun, China;2.Shenyang Institute of Geology and Mineral Resources, CGS, China;hengdu University of Technology, China);IDENTIFICATION OF ADAKITE-LIKE ROCKS IN THE MIDDLE JURASSIC VOLCANIC ROCKS FROM HAIFANGGOU FORMATION IN WEST LIAONING AREA AND ITS GEOLOGICAL SIGNIFICANCE[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-05
8 GAO Jian- guo1, XIA Ji- sheng1,CHENG Chang- yong2 (1.Kunming University of Science and Technology, Kunming 650093, China) ( 2.Kunming City Land Planning Bureau, Kunming 650093, China);GEOCHEMICAL FEATURES OF ALKALI-RICH PORPHYRY AND ANALYSIS OF AU (POLYMETALLIC)DEPOSITS IN WESTERN YUNNAN[J];GEOTECTONICA ET METALLOGENIA;2000-S1
9 XU Gui-zhong, ZHOU Rui, YAN Zhen, SHE Hong-quan, WANG Yi-fen, YANG Mao-sen, LI Bing (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Institute of Geophysical and Geochemical Prospecting, Shandong Province, Jinan;DISCUSSION ON THE EVIDENCES OF MESOZOIC LITHOSPHERE THINNING AND ITS DYNAMIC MECHANISM IN JIAODONG AREA[J];Geotectonica Et Metallogenia;2001-04
10 LI Chao wen1, 2, WANG Yue jun1, GUO Feng1, PENG Tou ping1,2 and YU Xiao bin1(1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Postgraduate School of the Chinese Academy of Sciences, Beijing 100039, China);GEOCHEMISTRY OF LATE MESOZOIC VOLCANIC ROCKS IN RUCHENG AREA AND ITS IMPLICATION FOR THE SOURCE NATURE[J];Geotectonica Et Metallogenia;2002-04
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