ScholarLens Back to search
2011•Geology and ResourcesRequires access

GENESIS OF THE COPPER-GOLD POLYMETALLIC DEPOSITS IN DAYAOSHAN OF GUANGXI,CHINA

Deng Jun

Open publisher page 3 citations

Abstract

The copper and gold deposits in Dayaoshan area of Guangxi Region occur mainly in Cambrian strata.The Cu-Au mineralization is genetically related to the Caledonian and Yanshanian tectonomagmatic activities.Based on the results of previous geological survey and researches,the metallogenic conditions for the Cu-Au polymetal deposits related to hypabyssal and super-hypabyssal igneous rocks are analyzed from the view of sedimentary formation,magmatic rock,tectonomagmatic activity,ore-forming fluid,trace element and sulfur isotopic characteristics.It is concluded that the deposits in the area genetically belong to sedimentary enrichment-fault structure-hydrothermal overlapping reformation type.The metallogenesis underwent early stage of sedimentary enrichment,middle stage of magmatic hydrothermal overlapping mineralization and end stage of post-magmatic fault and hydrothermal reformation.

About this research paper

What this paper is about

The copper and gold deposits in Dayaoshan area of Guangxi Region occur mainly in Cambrian strata.The Cu-Au mineralization is genetically related to the Caledonian and Yanshanian tectonomagmatic activities.Based on the results of previous geological survey and researches,the metallogenic conditions for the Cu-Au polymetal deposits related to hypabyssal and super-hypabyssal igneous rocks are analyzed from the view of sedimentary formation,magmatic rock,tectonomagmatic activity,ore-forming fluid,trace element and sulfur isotopic characteristics.It is concluded that the deposits in the area genetically belong to sedimentary enrichment-fault structure-hydrothermal overlapping reformation type.The metallogenesis underwent early stage of sedimentary enrichment,middle stage of magmatic hydrothermal overlapping mineralization and end stage of post-magmatic fault and hydrothermal reformation.

Why it matters

OpenAlex reports 3 citations for this work. Citation counts describe recorded attention and do not establish research quality.

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 copper and gold deposits in Dayaoshan area of Guangxi Region occur mainly in Cambrian strata.The Cu-Au mineralization is genetically related to the Caledonian and Yanshanian tectonomagmatic activities.Based on the results of previous geological survey and researches,the metallogenic conditions for the Cu-Au polymetal deposits related to hypabyssal and super-hypabyssal igneous rocks are analyzed from the view of sedimentary formation,magmatic rock,tectonomagmatic activity,ore-forming fluid,trace element and sulfur isotopic characteristics.It is concluded that the deposits in the area genetically belong to sedimentary enrichment-fault structure-hydrothermal overlapping reformation type.The metallogenesis underwent early stage of sedimentary enrichment,middle stage of magmatic hydrothermal overlapping mineralization and end stage of post-magmatic fault and hydrothermal reformation.

Key concepts: Geology, Mineralization (soil science), Geochemistry, Sedimentary rock, Hydrothermal circulation, Igneous rock, Skarn, Ore genesis

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
GENESIS OF THE COPPER-GOLD POLYMETALLIC DEPOSITS IN DAYAOSHAN OF GUANGXI,CHINA — Research Paper | ScholarLens