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《Geotectonica Et Metallogenia》 2006-01
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MINERAL CHEMISTRY AND GEOCHEMISTRY OF THE TWO SUITES OF PYROXENITE XENOLITHS IN CENOZOIC BASALTS FROM YANGYUAN, HEBEI

LIU Jiangfeng and Xu Yigang(CAS Key Laboratory of Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou, GD 510640, China)  
Cenozoic basalts in Yangyuan, Hebei, located in the west of the Daxing′anling-Taihangshan gravity lineament (DTGL), contain abundant peridotite and pyroxenite xenoliths. Two types of pyroxenite xenoliths are noted, namely, green Cr-and black Al-pyroxenites. All pyroxenites are websterites in which clinopyroxene is more abundant than orthopyroxene. Texture, major and trace element compositions suggest that the Yangyuan pyroxenites represent magmatic cumulates at high pressure. Their EMI-type Sr-Nd isotopic composition is different from that of the host basalts, ruling out the genetic relationship between them. It instead may have resulted from ancient magmatic events. Compilation of literature data reveals that the pyroxenite xenoliths collected from the west of DTGL are mostly characterized by enriched isotopic composition, whereas those from the east of DTGL show predominantly depleted isotopic composition. Such a spatial variation in pyroxenite composition, which supports the notion that the DTGL separates two different mantle domains, is likely related to the different formation ages of the lithospheric mantle beneath either side of the DTGL.
【Fund】: 中国科学院百人计划项目;; 国家杰出青年基金项目(编号:49925308)资助.
【CateGory Index】: P588.145
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9 Cheng Xiaojiu; Cheng Jingping; Wang Jianghai(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640);ELEMENT GEOCHEMISTRY OF SHOSHONITIC LAMPROPHYRES IN THE PENGJIAKUANG GOLD DISTRICT,SHANDONG PROVINCE, CHINA[J];Geochimica;1998-01
10 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
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