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- W2383215499 abstract "The Chimen bojite with a nearly NS strike,was a product of mafic magma activity in southeastern China at the end of Late Cretaceous.And it is spreaded in the northern part of Nanping City in Fujian Province.It belongs to low-K(tholeiite) rock series characterized by high Al contents and Na2OK2O,possibly resultant from fractional crystallization of olivine,clinopyroxene,plagioclase and titanium-iron oxide.These stocks are significantly enriched in LILE(such as K,Rb,Ba,Th,and U) and LREE,depleted in HFSE(Nb,Ta,Zr,Hf).In the primary mantle-normalized spidergram,they show the geochemical features of subduction-zone rocks and negative Nb,Ta,Ti anomalies.The results of trace element geochemical study indicated that the bojite was not contaminated by crustal material during emplacement it was derived from partial melting of garnet-free enriched lithospheric mantle,and the evolution of the mantle source region is closely related with the subduction of the Pacific plate.The Chimen bojite was formed in the geodynamic setting between the crustal extension belt and the continental initial rift.In combination with the results of geological studies for the Late Mesozoic mafic igneous rocks in SE China,it is suggested that the Chimen bojite belongs to the transitional rock series in the transitional zone from the crustal extension belt to the continental initial rift,which may be used to trace rift start up when compared to the coastal gabbro." @default.
- W2383215499 created "2016-06-24" @default.
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- W2383215499 date "2009-01-01" @default.
- W2383215499 modified "2023-09-25" @default.
- W2383215499 title "GEOCHEMICAL CHARACTERISTICS OF BOJITE IN NORTHERN FUJIAN PROVINCE AND THEIR GEODYNAMIC SIGNIFICANCE" @default.
- W2383215499 hasPublicationYear "2009" @default.
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