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《Geochimica》 2004-01
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Petrology and geochemistry of the Cenozoic basalts from Yangyuan of Hebei Province and Datong of Shanxi Province:Implications for the deep process in the western North China Craton

MA Jin-long,XU Yi-gang (Guangzhou Institute of Geochemistr y,Chinese Academy of Sciences,Guan gz hou510640,China)  
Major and trace element composition s and Sr-Nd isotopes of the C enozoic b asalts from Yangyuan(Hebei Province)and Datong(Shanxi Province),w hich are located to west of the Da Hi nggan Ling-Taihangshan gravity gradient z one,are reported.The Early Tertiary alkali basalts from Yangyuan contain abund ant mantle xenoliths.They exhibit very homogeneous Sr-Nd isotopes with? Nd =5.7,and their trace elements resem ble those of ocean island basalts. Therefore,they mainly originated from the asthenospheric mantle at a relatively great dept h.At Datong,the Quaternary basalts include both alkali and tholei itic types.The Datong alkali basalts were also generated within the asthenosphe ric mantle but at a shallow depth compared to the Yangyuan alkali basalts.The D atong tholeiitic basalts exhibit l ow? Nd values(1~4),implying the effect of the asthenosphere-lithosphere inte ractions.These magmas were derived from a shallower depth than the a lkali basa lts.The distinct spatial distribution of the tholeiitic and a lkali basalts at Datong may be relate d to the effect of local lithospheric extension on the pass ive upwelling of asthenosphere and variable extents of interaction between litho sphere and asthenosphere.
【Fund】: 国家杰出青年基金项目(49925308)
【CateGory Index】: P588.1
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