甘肃花牛山铅锌矿床闪锌矿LA-ICP-MS微量元素组成及其地质意义

doi:10.13278/j.cnki.jjuese.20190293

Abstract

Abstract: Tianshan-Beishan Pb-Zn metallogenic belt is located in the intersection of Central Asian orogenic belt, Tarim Craton,and North China craton, which is one of the important metal resources in Northwest China. Huaniushan Pb-Zn deposit is a typical genetic deposit in Tianshan-Beishan area. The results of LA-ICP-MS analysis on the trace element composition of sphalerite show that the sphalerite was formed in the medium-high temperature environment and characterized by rich in Fe, Mn, Cd, In, Cu and poor in Ga,Ge,Ni. Among them, Mn, Fe, In, Cd, Cu are in the lattice of sphalerite in the form of isomorphism, whereas Ag and Pb may exist in the form of micro-inclusions. The trace element composition is similar to that of the magmatic hydrothermal deposits (Dulong, Huanggangliang, Meng'entaolegai,Chitudian);in addition, the mass fraction of Tl element and the values of Cd/Fe and Cd/Mn of sphalerite show magmatic hydrothermal properties, and the trace element discrimination figure also falls into magmatic hydrothermal region. The field investigation shows that there are no brecciated or reticular ore bodies at the bottom of the deposit, and the ore bodies are developed in the lithologic interfaces and interlayer fracture zones. Based on the geological characteristics of the deposit and the geochemistry of sphalerite, it is conclude that the genetic type of Huaniushan Pb-Zn deposit belongs to magmatic hydrothermal type formed at medium-high temperature.

Key words: Tianshan-Beishan Pb-Zn metallogenic belt, Huaniushan Pb-Zn deposit, sphalerite, trace elements, LA-ICP-MS

CLC Number:

P618.42

Kang Kai, Du Zezhong, Yu Xiaofei, Li Yongsheng, Lü Xin, Sun Hairui, Du Yilun. LA-ICP-MS Trace Element Analysis of Sphalerite in Huaniushan Pb-Zn Deposit in Gansu Province and Its Geological Significance[J].Journal of Jilin University(Earth Science Edition), 2020, 50(5): 1418-1432.

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LA-ICP-MS Trace Element Analysis of Sphalerite in Huaniushan Pb-Zn Deposit in Gansu Province and Its Geological Significance

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