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《GEOCHIMICA》 2000-04
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Geochronology of cumulate xenoliths and their host diorites from Harqin, eastern Nei Mongol

SHAO Ji an1, ZHANG Ren hu2, HAN Qing jun2, ZHANG Lü qiao3,QIAO Guang sheng2, SANG Hai qing2(1 Department of Geology, Peking University, Beijing 100871, China; 2 Institute of Geology and Geophysics, Chinese Academy of Science, Beijing 100029, Ch  
Harqin area is located in a joint place of Mesozoic tectono magmatic belt in the Da Hinggan Mts. and North China craton. Mafic ultramafic cumulate xenoliths with various lithological population including pyroxenite, gabbro,norite, hornblendite and anorthorsite as well as basic granulite xenoliths occurred in a series of diorite which intruded into Archean metamorphic rocks in thearea, and these xenoliths are interpreted as products of mantle derived basaltic underplating. Isotopic ages of the cumulate xenoliths and their host dioritehave been systematically measured by means of whole rock Rb Sr isochron, K Ar and 40Ar 39Ar techniques and 8 ages are obtained. Two whole rock Rb Sr isochron ages for olivine pyroxenite are (229±23) Ma with initial 87Sr/86Sr ratios of 0 705 54±0 000 12, respectively. 40Ar 39Ar dating of plagioclase from anorthorsite yields a plateau age of (228±1) Ma and an isochron age of (240±5) Ma with 40Ar/36Ar initial ratio of 290; 40Ar 39Ar dating of plagioclasefrom norite yields a plateau age of (230±2) Ma and an isochron age of (232±6) Ma with 40Ar/36Ar initial ratio of 296 very near to that of atmospheric argon(Neir value = 295 5), indicating these ages are reasonable. K Ar ages of plagioclase from anorthorsite and hornblende from hornblendite are (237 4±8) Ma and (220 9±4 1) Ma, respectively, suggesting that they are not products of fractionational crystalline from the same patch of magma. K Ar ages of whole rockand hornblende single mineral from diorites, the host of cumulate xenoliths, range from (218 5±4 5) Ma to (223 3±3 3) Ma, indicating that the diorite cooled at a high rate from (530±40) ℃(closure temperature of K Ar systematics for hornblende) down to about 200 ℃(closure temperature of K Ar systematicsfor whole rock), inferring a tectonic environment of uplifting at a relatively high rate for North China craton in the Early Mesozoic.
【Fund】: 国家自然科学基金资助项目!(49272156)
【CateGory Index】: P597
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4 ZHANG Qi,WANG Yan,PAN GuoQiang,LI CenDong and JIN WeiJun 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China 3.Department of Earth Sciences,Nanjing University,Nanjing 210093,China 4.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China;Sources of granites:some crucial questions on granite study(4)[A];[C];2009
5 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
6 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
7 CHEN WeiJun~(1,2),LIU JianMing~1,LIU HongTao~1,SUN XingGuo~(1,2),ZHANG RuiBin~(1,2),ZHANG ZuoLun~(1,2) and QIN Feng~(1,2) 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;Geochronology and fluid inclusion study of the Jiguanshan porphyry Mo deposit,Inner Mongolia[A];[C];2011
8 WU HuaYing~(1,2),ZHANG LianChang~1,CHEN ZhiGuang~(1,2),WAN Bo~(2,3),XIANG Peng~(1,2) and ZHANG XiaoJing~(1,2) 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 3.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Hypersaline,high-oxygen fugacity and F-rich fluid inclusions in Jiguanshan porphyry molybdenum deposit,Xilamulun metallogenic belt.1374[A];[C];2011
9 ZHANG LianChang,WU HuaYing,XIANG Peng,ZHANG Xiaojing,CHEN ZhiGuang and WAN Bo Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Ore-forming processes and mineralization of complex tectonic system during the Mesozoic:A case from Xilamulun Cu-Mo metallogenic belt[A];[C];2011
10 ZHANG XiaoJing~(1,2),ZHANG LianChang~1,JIN XinDi~1,WU HuaYing~(1,2),XIANG Peng~(1,2) and CHEN ZhiGuang~(1,2) 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;U-Pb ages,geochemical characteristics and their implications of Banlashan molybdenum deposit[A];[C];2011
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