Fluid inclusions and H–O–C–S isotope constraints on fluid evolution and ore genesis of the Wangjiadashan Cu–Au deposit in Suizao area of the Tongbai‐Dabie orogenic belt, central China
Abstract
The Wangjiadashan Cu–Au deposit is a vein-type deposit controlled by the secondary faults of the Wushan Fault zone in the Suizao area of Hubei Province. Three hydrothermal stages are identified, namely, (I) barren quartz stage, (II) the quartz-sulphide stage, and (III) quartz-carbonate stage. Six types of fluid inclusions occur in quartz: (a) liquid-rich aqueous fluid inclusions (L + V), (b) vapour-rich aqueous-carbonic fluid inclusions (V + L),...
Paper Details
Title
Fluid inclusions and H–O–C–S isotope constraints on fluid evolution and ore genesis of the Wangjiadashan Cu–Au deposit in Suizao area of the Tongbai‐Dabie orogenic belt, central China
Published Date
Apr 15, 2019
Journal
Volume
55
Issue
2
Pages
1563 - 1586
Citation AnalysisPro
You’ll need to upgrade your plan to Pro
Looking to understand the true influence of a researcher’s work across journals & affiliations?
- Scinapse’s Top 10 Citation Journals & Affiliations graph reveals the quality and authenticity of citations received by a paper.
- Discover whether citations have been inflated due to self-citations, or if citations include institutional bias.
Notes
History