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Cenozoic Volcanism in Tibet: Evidence for a Transition from Oceanic to Continental Subduction 总被引:93,自引:2,他引:93
Geochronological (KAr or 40Ar/39Ar), major and traceelement, SrNdPb isotopic and mineral chemicaldata are presented for newly discovered Cenozoic volcanic rocksin the western Qiangtang and central Lhasa terranes of Tibet.Alkali basalts of 6545 Ma occur in the western Qiangtangterrane and represent primitive mantle melts as indicated byhigh mg-numbers [100 x Mg/(Mg + Fe)] (5465), Cr (204839ppm) and Ni (94218 ppm) contents, and relatively lowratios of 87Sr/86Sr (0·70460·7061), 206Pb/204Pb(18·2118·89), 207Pb/204Pb (15·4915·61)and 208Pb/204Pb (38·4238·89), and highratios of 143Nd/144Nd (0·51240·5127). Incontrast, younger volcanic rocks in the western Qiangtang terrane( 相似文献
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HAO NANA YUAN WANMING ZHANG AIKUI FENG YUNLEI CAO JIANHUI CHEN XIAONING CHENG XUEQIN MO XUANXUE 《Journal of Earth System Science》2015,124(1):171-196
Journal of Earth System Science - The East Kunlun Orogenic Belt has undergone a composite orogenic process consisting of multiple orogenic cycles and involving many types of magmatic rocks spread... 相似文献
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ZHIXIN HUANG WANMING YUAN CHANGMING WANG XIANGWEI LIU XIAOTONG XU LIYA YANG 《Journal of Earth System Science》2012,121(6):1401-1420
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