ScholarLens Back to search
2009•Geology and ResourcesRequires access

CHARACTERISTICS OF ORE AND OCCURRENCE OF GOLD OF THE WANGJIAWAIZI GOLD DEPOSIT IN LIAONING PROVINCE, CHINA

Bian Guang-qing

Open publisher page 1 citations

Abstract

The Wangjiawaizi gold deposit is situated in the southeast of Yingkou City, Liaoning Province. The ore of the gold deposit is dominated by gold-bearing quartz vein type, with rich pyrite as main gold-carrier. The pyrite, closely related to gold mineralization in time, space and genesis, is the significant indicator for the metallogenesis of gold. The ore is in heterogranular and metasomatic dissolution textures and massive, dense massive and veinlet-disseminated structures. The gold minerals are medium- to fine-grained electrum and goldargentid in complicated shapes, occurring in fissures, crystal cracks and inclusions. The gold-carrying minerals include pyrite, galena, sphalerite, chalcopyrite and quartz. The deposit is characterized by metamorphic hydrothermal type. The multi-sourced mesothermal and meso-epithermal fluid is the major ore-forming factor.

About this research paper

What this paper is about

The Wangjiawaizi gold deposit is situated in the southeast of Yingkou City, Liaoning Province. The ore of the gold deposit is dominated by gold-bearing quartz vein type, with rich pyrite as main gold-carrier. The pyrite, closely related to gold mineralization in time, space and genesis, is the significant indicator for the metallogenesis of gold. The ore is in heterogranular and metasomatic dissolution textures and massive, dense massive and veinlet-disseminated structures. The gold minerals are medium- to fine-grained electrum and goldargentid in complicated shapes, occurring in fissures, crystal cracks and inclusions. The gold-carrying minerals include pyrite, galena, sphalerite, chalcopyrite and quartz. The deposit is characterized by metamorphic hydrothermal type. The multi-sourced mesothermal and meso-epithermal fluid is the major ore-forming factor.

Why it matters

OpenAlex reports 1 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 Wangjiawaizi gold deposit is situated in the southeast of Yingkou City, Liaoning Province. The ore of the gold deposit is dominated by gold-bearing quartz vein type, with rich pyrite as main gold-carrier. The pyrite, closely related to gold mineralization in time, space and genesis, is the significant indicator for the metallogenesis of gold. The ore is in heterogranular and metasomatic dissolution textures and massive, dense massive and veinlet-disseminated structures. The gold minerals are medium- to fine-grained electrum and goldargentid in complicated shapes, occurring in fissures, crystal cracks and inclusions. The gold-carrying minerals include pyrite, galena, sphalerite, chalcopyrite and quartz. The deposit is characterized by metamorphic hydrothermal type. The multi-sourced mesothermal and meso-epithermal fluid is the major ore-forming factor.

Key concepts: Pyrite, Geology, Sphalerite, Mesothermal, Geochemistry, Chalcopyrite, Galena, Mineralization (soil science)

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
CHARACTERISTICS OF ORE AND OCCURRENCE OF GOLD OF THE WANGJIAWAIZI GOLD DEPOSIT IN LIAONING PROVINCE, CHINA — Research Paper | ScholarLens