Magmatic-hydrothermal fluid evolution of the tin-polymetallic metallogenic systems from the Weilasituo ore district, Northeast China

Magmatic-hydrothermal fluid evolution of the tin-polymetallic metallogenic systems from the Weilasituo ore district, Northeast China

Abstract The large Weilasituo Sn-polymetallic deposit is a recent exploration discovery in the southern Great Xing’an Range, northeast China. The ore cluster area shows horizontal mineralization zoning, from the inner granite body outward, consisting of high-T Sn–W–Li mineralization, middle-T Cu–Zn...

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Bibliographic Details
Main Authors: Xu Gao, Zhenhua Zhou, Karel Breiter, Jingwen Mao, Rolf L. Romer, Nigel J. Cook, François Holtz
Format: Article
Language:English
Published: Nature Portfolio 2024-02-01
Series:Scientific Reports
Subjects:
In situ LA-ICP-MS trace element analysis
H-O isotopes
Fluid mixing
Physico-chemical conditions
Sn-polymetallic ore systems
Online Access:https://doi.org/10.1038/s41598-024-53579-y

Internet

https://doi.org/10.1038/s41598-024-53579-y

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