2021•Unpublished venueRequires access

Characteristics of the hydrothermal system of the porphyry copper (gold) deposit at Shaxi, Eastern China

Qijang Ren, Bing Fu, Wenxuan Hu, Wenyi Xu, Zhenhao Duan, Nancy Møller, John H. Weare

Open publisher page 0 citations

Abstract

The porphyry copper (gold) deposit at Shaxi is a special and large size deposit in eastern China. In the ore-forming process, the water and ore-forming materials in ore solution were magmatic in origin. Systematic studies of fluid inclusions reveal that the ore-forming system was characterized by relatively high temperature and low pressure as well as high contents of CO 2 and NaCl. Great amounts of evidence support that the fluid immiscibility played an important part in the formation of Shaxi porphyry copper (gold) deposits.

About this research paper

What this paper is about

The porphyry copper (gold) deposit at Shaxi is a special and large size deposit in eastern China. In the ore-forming process, the water and ore-forming materials in ore solution were magmatic in origin. Systematic studies of fluid inclusions reveal that the ore-forming system was characterized by relatively high temperature and low pressure as well as high contents of CO 2 and NaCl. Great amounts of evidence support that the fluid immiscibility played an important part in the formation of Shaxi porphyry copper (gold) deposits.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The porphyry copper (gold) deposit at Shaxi is a special and large size deposit in eastern China. In the ore-forming process, the water and ore-forming materials in ore solution were magmatic in origin. Systematic studies of fluid inclusions reveal that the ore-forming system was characterized by relatively high temperature and low pressure as well as high contents of CO 2 and NaCl. Great amounts of evidence support that the fluid immiscibility played an important part in the formation of Shaxi porphyry copper (gold) deposits.

Key concepts: China, Hydrothermal circulation, Porphyry copper deposit, Geochemistry, Geology, Copper, Metallurgy, Geography

Related papers

Back to paper searchBrowse research topicsOriginal source
Characteristics of the hydrothermal system of the porphyry copper (gold) deposit at Shaxi, Eastern China — Research Paper | ScholarLens