作者: Chu-Nan Hsu , Ju-Chin Chen , Kung-Suan Ho
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摘要: The major volcanic activity in Kirin Province, northeast China occurred Changpaishan area and lasted from the Miocene to Holocene. rocks include basanite, alkali basalt, tholeiite, trachyte, rhyolite. Ultramafic xenoliths megacrysts occur basanite basalt. compatible (Ni, Cr, Sc, V, Co) incompatible elements (Rb, Li, Th, Hf, La, Lu, Nb, Zr, Y) vary systematically with 100MgO/(MgO + ΣFeO) rocks. Fractional crystallization clearly was important magmatic evolution. their ultramafic have characteristic Sr Nd isotopic ratios which fall between DMM EM-I or EM-II. There are two types of spinel-lherzolite basalts Province: (1) an E-type enriched LREE (La/Yb)N varying 6.6 8.15; (2) a D-type depleted 0.2 0.7 indicating mantle heterogeneity region. lherzolites contain higher TiO2, K2O, P2O5, Rb, Sr, Ba, Y, Ta, Th U than lherzolites. former may resulted metasomatic processes. basalt been derived isotopically similar source through different degree partial melting at P-T conditions. trachyte be fractional plagioclase, olivine, clinopyroxene magnetite.