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Sub-solidus hydrology controls the formation of high-grade tin deposits in granites
N
J
P
T
DOI:10.1016/j.epsl.2026.120186.png)
Abstract
En 中文
• Efficient sub-solidus metal mobilisation and fluid focusing in granitic intrusions. • Post-crystallisation storage of magmatic fluids in the crystallised ductile granite. • Modelled fluid evolution matches field-based observations in tin deposits. • Different tin precipitation mechanisms result from the same hydrological process.
Keywords:
Tin deposits
Magmatic hydrothermal systems
Numerical fluid flow modelling
Journal
IF:
5.1
Papers:
774
Citations:
6.9W
