Browsing by Author "Xiao W.J."
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Browsing by Author "Xiao W.J."
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Li Z.L.; Chen H.L.; Yang S.F.; Xiao W.J.; Tainosho Y. (2004)The Altay mafic granulite (AMG). representing metamorphic product of granulite-facies in the lower crust, was first found in the Fuyun Wuqiagou, Altay progenic bell through detailed field survey and mineral-chemical study. ...
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Xiao W.J.; Windley B.F.; Huang B.C.; Han C.M.; Yuan C.; Chen H.L.; Sun M.; Sun S.; Li J.L. (2009)The Altaids is one of the largest accretionary orogenic collages in the world with the highest rate of Phanerozoic continental growth and significantmetallogenic importance. It is widely accepted that subduction-related ...
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Long X.P.; Yuan C.; Zhao Y.J.; Cai K.D.; Sun M.; Xiao W.J.; Li J.L.; Chen H.L. (2006)Zhaheba Carboniferous volcanic rocks mainly composed of basalts and basaltic andesites occur within Upper Carboniferous Batamayi Group, north of Zhaheba ophiolite in the eastern Junggar. These rocks have relatively high ...
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Han C.M.; Xiao W.J.; Mao Q.G.; Zhao G.C.; Qu W.J.; Du A.D. (2006)The Kalatongke is a large Cu-Ni deposit in the southern part of the Altay orogenic belt, northwestern China. Rhenium and osmium isotopic analyses of Ni-and Cu-bearing sulfide minerals from the deposit have been used to ...
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Windley B.F.; Xiao W.J. (Федеральное государственное бюджетное учреждение науки Институт земной коры Сибирского отделения Российской академии наук, 2017)
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Mao Q.G.; Xiao W.J.; Han C.M.; Yan Z.; Yong Y.; Zhang J.E.; Yuan C.; Sun M.; Li J.L. (2006)The Baishiquan Cu-Ni sulfide deposit is located in the northern part of the Center Tianshan Massif, south of the Aqikuduke-Shaquanzi fault of the Eastern Tianshan Mountains. Ore-body was formed by the magmas and lay within ...
Now showing items 1-6 of 6