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- W2380442908 abstract "The volcanic rocks from the Liushugou formation are widely distributed in Balikuntage area,Xinjiang.Study on the basalt,their petrology,geochemistry and isotope geochemistry indicate that,the basalts in this area belong to tholeiite series and are characterized by LREE,LILE(Sr,K,Rb,Ba,Th) enrichments and HFSE(Nb,Ta,Ti),HREE depletion,low Sr-Nd-Pb isotope(~(87)Sr/~(86)Sr) t = 0.70382-0.70667;(~(206)Pb/~(204) Pb) t= 17.857-18.054;(~(207)Pb/~(204)Pb) t =15.494-15.545;(~(208)Pb/~(204)Pb) t = 37.746-37.798 and high eNd(eNd_(t)= + 4-+ 8.3),which show its depleted mantle origin and contamination of crust materials.Through comparing with the basalts of the eastern Bogda in the same period,the results show that Balikuntage has the similar structure attributes with the Bogda area,which is the continental rifting in the late Carboniferous.But they belong to different stages of rifting evolution,thus,their geochemistry exhibits some disparities." @default.
- W2380442908 created "2016-06-24" @default.
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- W2380442908 date "2015-01-01" @default.
- W2380442908 modified "2023-09-26" @default.
- W2380442908 title "Genesis and Tectonic Environment of Basalts in Balikuntage,Xinjiang:Implications from Geochemistry and Sr-Nd-Pb Isotopes" @default.
- W2380442908 hasPublicationYear "2015" @default.
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