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

Volume: 55, Issue: 2, Pages: 1563 - 1586
Published: Apr 15, 2019
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
Volume
55
Issue
2
Pages
1563 - 1586
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