Fault-fluid evolution in the Xitian W–Sn ore field (South China): Constraints from scheelite texture and composition

Volume: 114, Pages: 103140 - 103140
Published: Nov 1, 2019
Abstract
Understanding fault-fluid evolutionary processes is crucial for understanding the genesis of vein-type deposits. Scheelite and quartz are common hydrothermal minerals in W–Sn ore field faults. In the Xitan ore field (Nanling Range, South China), scheelite textural and compositional features were studied and two types of scheelite were identified: Type I (represented by scheelite in the Xihu fault) is intergrown with quartz, has oscillatory...
Paper Details
Title
Fault-fluid evolution in the Xitian W–Sn ore field (South China): Constraints from scheelite texture and composition
Published Date
Nov 1, 2019
Volume
114
Pages
103140 - 103140
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