ScholarLens Back to search
2001•Xinjiang GeologyRequires access

GEOLOGICAL CHARCTERISITC AND PRELIMINARY STUDY ON GENESIS OF SAERSUOC GOLD DEPOSIT

Xiaobing Wang

Open publisher page 0 citations

Abstract

Saersoc gold deposit occures in the acid-intermediateacid volcanics-subvolcanics of the Ashele formation in middle Devonian. The morphology and special listribution of the ore body are strictly controlled by the NNW pressure and torsion fractures. The main ore body ,in veined and lenricular shape, is dipping at the angle of 60-87. The ores mainly of alteration type follower by quartz vein type. The country rocks are rhyolith showing beresitization alteration. The origin of ore deposit is in close relationshop with paleovolcanic apparatus, subvolcanic and fracture structures. So saersuoc gold deposit is believed to be of volcanic-subvolcanic hydrothermal type of low to inter mediate-temperature .

About this research paper

What this paper is about

Saersoc gold deposit occures in the acid-intermediateacid volcanics-subvolcanics of the Ashele formation in middle Devonian. The morphology and special listribution of the ore body are strictly controlled by the NNW pressure and torsion fractures. The main ore body ,in veined and lenricular shape, is dipping at the angle of 60-87. The ores mainly of alteration type follower by quartz vein type. The country rocks are rhyolith showing beresitization alteration. The origin of ore deposit is in close relationshop with paleovolcanic apparatus, subvolcanic and fracture structures. So saersuoc gold deposit is believed to be of volcanic-subvolcanic hydrothermal type of low to inter mediate-temperature .

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

Saersoc gold deposit occures in the acid-intermediateacid volcanics-subvolcanics of the Ashele formation in middle Devonian. The morphology and special listribution of the ore body are strictly controlled by the NNW pressure and torsion fractures. The main ore body ,in veined and lenricular shape, is dipping at the angle of 60-87. The ores mainly of alteration type follower by quartz vein type. The country rocks are rhyolith showing beresitization alteration. The origin of ore deposit is in close relationshop with paleovolcanic apparatus, subvolcanic and fracture structures. So saersuoc gold deposit is believed to be of volcanic-subvolcanic hydrothermal type of low to inter mediate-temperature .

Key concepts: Geology, Devonian, Geochemistry, Quartz, Hydrothermal circulation, Volcanic rock, Vein, Volcano

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
GEOLOGICAL CHARCTERISITC AND PRELIMINARY STUDY ON GENESIS OF SAERSUOC GOLD DEPOSIT — Research Paper | ScholarLens