The influence of deformation and metamorphism of post volcanic massive sulfide on the trace elements and sulfur lead isotopic composition of sulfide is still unclear. The Keketale VMS Pb Zn (- Ag) deposit provides an opportunity to solve the above problems; Five ore samples from No.7 and No.9 orebodies were crushed and screened for lead isotope analysis of bulk minerals, 17 polished thick sulfide samples were used for in-situ trace element and sulfur lead isotope analysis, 66 trace element determination points were analyzed, and 25 sulfur isotope points were determined; A total of 18 point pairs of different minerals were selected for lead isotope analysis, and LA-ICP-MS method was used

File naming and required software

File name: KEKETALE lead-zinc deposit trace elements, sulfur lead isotope data set, the name of the file is "KEKETALE trasl. Xlsl", in which KEKETALE represents KEKETALE lead-zinc deposit, trasl trace elements, sulfur lead isotope
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Cite as:

Yu, P., Zheng, Y. (2021). Data set of trace elements, sulfur and lead isotopes in KEKETALE lead zinc deposit. A Big Earth Data Platform for Three Poles, DOI: 10.1016/j.oregeorev.2020.103685. (Download the reference： RIS | Bibtex )

Related Literatures:

1. Yu, P.P., Zheng, Y., Wang, C.M. (2020). Trace elemental and sulfur-lead isotopic variations in metamorphosed volcanogenic massive sulfide (VMS) mineralization systems: An example from the Keketale Pb-Zn(-Ag) deposit, NW China. Ore Geology Reviews,125, 103685.( View Details | Bibtex)

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.

Support Program

Deep processes and resource effects of major geological events during the Yan Mountains period (No:2016YFC0600400)

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