1999Journal of Hefei University of TechnologyRequires access

Geological characteristics and genesis of the silver deposit at Xikeng in Yixian County, Southern Anhui Province

Chen Tian

Open publisher page 0 citations

Abstract

This paper studies the deposit′s geological characteristics such as the shape of silver ore body,ore composition, texture and structure,ore forming physical and chemical condition ,existing forms of silver in the ore,and magmatism at the mine area.The stratous geochemistry of the mine area and far from the mine area is also studied. According to the study of the stratous geochemistry and geological characteristic of the deposit,the author thinks that it is a continuous process of thermal event of magmatism from thermal metamorphism of pro metallizing,tremolite diopside forming at early term to sulfidization at late term.The ore forming material comes from magmatic fluid.While acid magmatic fluid rises along zone of fracture in the mid stratum, the ore forming material fills up the fracture because of the reaction between the magmatic fluid and rock which is high active and rich incarbonate.

About this research paper

What this paper is about

This paper studies the deposit′s geological characteristics such as the shape of silver ore body,ore composition, texture and structure,ore forming physical and chemical condition ,existing forms of silver in the ore,and magmatism at the mine area.The stratous geochemistry of the mine area and far from the mine area is also studied. According to the study of the stratous geochemistry and geological characteristic of the deposit,the author thinks that it is a continuous process of thermal event of magmatism from thermal metamorphism of pro metallizing,tremolite diopside forming at early term to sulfidization at late term.The ore forming material comes from magmatic fluid.While acid magmatic fluid rises along zone of fracture in the mid stratum, the ore forming material fills up the fracture because of the reaction between the magmatic fluid and rock which is high active and rich incarbonate.

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

This paper studies the deposit′s geological characteristics such as the shape of silver ore body,ore composition, texture and structure,ore forming physical and chemical condition ,existing forms of silver in the ore,and magmatism at the mine area.The stratous geochemistry of the mine area and far from the mine area is also studied. According to the study of the stratous geochemistry and geological characteristic of the deposit,the author thinks that it is a continuous process of thermal event of magmatism from thermal metamorphism of pro metallizing,tremolite diopside forming at early term to sulfidization at late term.The ore forming material comes from magmatic fluid.While acid magmatic fluid rises along zone of fracture in the mid stratum, the ore forming material fills up the fracture because of the reaction between the magmatic fluid and rock which is high active and rich incarbonate.

Key concepts: Magmatism, Geology, Diopside, Geochemistry, Tremolite, Metamorphism, Stratum, Fracture (geology)

Related papers

Back to paper searchBrowse research topicsOriginal source
Geological characteristics and genesis of the silver deposit at Xikeng in Yixian County, Southern Anhui Province — Research Paper | ScholarLens