Data for: The formation of a magmatic Ni–Cu sulfide deposit in mafic intrusions at the Kalatongke, NW China: Insights from amphibole mineralogy and composition

Published: 31-03-2020| Version 1 | DOI: 10.17632/rb4d3xbr74.1
Contributor:
Kezhang Qin

Description

Table 1. Major-element compositions (wt.%) of amphiboles from the Kalatongke and Eastern Tianshan intrusions. Data for the Xiangshanzhong intrusions are from Jiang et al. (2014). Table 2. Trace-element compositions (ppm) of amphiboles from the Kalatongke and Eastern Tianshan intrusions. Table 3. Trace-element compositions (ppm) of clinopyroxenes from the Kalatongke intrusions. Table 4. Results of FTIR analysis of clinopyroxenes from the Kalatongke intrusions. Table 5. Whole-rock major- and trace-element compositions of the Kalatongke mafic–ultramafic intrusions. Table 6. Average compositions of modeled melts in equilibrium with clinopyroxenes from the pyroxenite (Melt 1), with amphiboles from the diorite at the margin of the Y1 intrusion (Melt 2a), and with amphiboles from the olivine norite or norite (Melt 2b). Table 7. Major-element compositions (wt.%) of clinopyroxenes from the Kalatongke intrusions. Appendix 1.Whole-rock major- and trace-element compositions of the Kalatongke mafic–ultramafic intrusions. Appendix 2. Trace element compositions (ppm) of NIST 610 in this study

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