Magmatism and mineralization in the Permian large igneous province in the Tarim Basin, NW China
The Early Permian Tarim Large Igneous Province (Tarim LIP) in northwestern China, contains extensive flood basaltic lavas, interlayered with tuff and sedimentary rocks, and layered intrusive rocks.The lavas have ages of 290-285 Ma, whereas the intrusive rocks range from 284 to 2 74 Ma.Using whole-rock geochemistry and Sr-Nd-Pb-Hf-PGE isotopic data of the different magmatic rock types and the associated Fe-Ti-V oxide deposit, we present a magmatic evolutionary model for the Tarim LIP genetically relating it to mantle plume activity and discuss the genesis of the Wajilitag Fe-Ti-V oxide deposit.
Spatial-temporal distribution Sr-Nd-Pb-Hf isotopes magma source and evolution Fe-Ti oxides Tarim large igneous province Permian
Zilong Li Yinqi Li Shufeng Yang Hanlin Chen Yu Xing Siyuan Zou
Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
国际会议
武汉
英文
32-33
2014-10-11(万方平台首次上网日期,不代表论文的发表时间)