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July 23, 2025

Supplemental Material: Pyroxenite source for the ultramafic–mafic intrusions in the giant Xiarihamu Cu-Ni sulfide deposit, China

Shirong Chen et al.

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Key Points

MAIN FINDING: The study identifies a pyroxenite source for ultramafic-mafic intrusions in the Xiarihamu Cu-Ni sulfide deposit.
KEY EVIDENCE: Geological surveys and mineral analyses confirm the relationship between pyroxenite and copper-nickel sulfide formations.
APPROACH: Detailed field mapping and mineral composition studies were conducted in the Xiarihamu region to establish geological connections.
SIGNIFICANCE: Understanding the source of these intrusions may enhance exploration strategies for Cu-Ni resources globally.

Implication

Research uncovers pyroxenite origins for ultramafic-mafic intrusions in Xiarihamu Cu-Ni deposit, suggesting significant geological implications.

Abstract

Pyroxenite source for the ultramafic–mafic intrusions in the giant Xiarihamu Cu-Ni sulfide deposit, China

Discussion

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Cite This Study

Chen et al. (2025) studied this question.

synapsesocial.com/papers/689a0621e6551bb0af8cddf0 https://doi.org/10.1130/gsab.s.29627528

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Keep reading

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

1Supplemental Material: Pyroxenite source for the ultramafic–mafic intrusions in the giant Xiarihamu Cu-Ni sulfide deposit, China2025
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