2011•Geology and ResourcesRequires access

METALLOGENIC RULES AND PROSPECTING ORIENTATION OF GOLD DEPOSIT IN THE DUOBAOSHAN AREA,HEILONGJIANG PROVINCE

Li Cheng

Open publisher page 3 citations

Abstract

Based on the studies of the geology and geochemistry of typical gold deposits,as well as the distribution and genesis of gold deposits and occurrences in the Duobaoshan area of Heilongjiang Province,the gold metallogenic rule is analyzed.The results show that the gold mineralization is controlled by NW-and NE-trending faults,of which the NE-trending faults are dominated.From west to east,the gold mineralization is becoming stronger.The ore bodies are hosted in the Middle Ordovician and Early Yanshanian volcanic rocks,with ore-forming materials from mainly Yanshanian magmatic rocks and wallrocks.The ore-forming fluids are mainly from meteoric water.The homogenization temperature of fluid inclusions ranges from 133℃ to 267℃.The genesis of the gold deposits in the area belongs to typical epi-mesothermal ore deposit.At last,some prospecting criteria are proposed for the further exploration in the area and the prospecting orientations are determined.

About this research paper

What this paper is about

Based on the studies of the geology and geochemistry of typical gold deposits,as well as the distribution and genesis of gold deposits and occurrences in the Duobaoshan area of Heilongjiang Province,the gold metallogenic rule is analyzed.The results show that the gold mineralization is controlled by NW-and NE-trending faults,of which the NE-trending faults are dominated.From west to east,the gold mineralization is becoming stronger.The ore bodies are hosted in the Middle Ordovician and Early Yanshanian volcanic rocks,with ore-forming materials from mainly Yanshanian magmatic rocks and wallrocks.The ore-forming fluids are mainly from meteoric water.The homogenization temperature of fluid inclusions ranges from 133℃ to 267℃.The genesis of the gold deposits in the area belongs to typical epi-mesothermal ore deposit.At last,some prospecting criteria are proposed for the further exploration in the area and the prospecting orientations are determined.

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

Based on the studies of the geology and geochemistry of typical gold deposits,as well as the distribution and genesis of gold deposits and occurrences in the Duobaoshan area of Heilongjiang Province,the gold metallogenic rule is analyzed.The results show that the gold mineralization is controlled by NW-and NE-trending faults,of which the NE-trending faults are dominated.From west to east,the gold mineralization is becoming stronger.The ore bodies are hosted in the Middle Ordovician and Early Yanshanian volcanic rocks,with ore-forming materials from mainly Yanshanian magmatic rocks and wallrocks.The ore-forming fluids are mainly from meteoric water.The homogenization temperature of fluid inclusions ranges from 133℃ to 267℃.The genesis of the gold deposits in the area belongs to typical epi-mesothermal ore deposit.At last,some prospecting criteria are proposed for the further exploration in the area and the prospecting orientations are determined.

Key concepts: Prospecting, Mesothermal, Geology, Geochemistry, Mineralization (soil science), Ordovician, Gold ore, Meteoric water

Related papers

Back to paper searchBrowse research topicsOriginal source
METALLOGENIC RULES AND PROSPECTING ORIENTATION OF GOLD DEPOSIT IN THE DUOBAOSHAN AREA,HEILONGJIANG PROVINCE — Research Paper | ScholarLens