Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration

被引:0
|
作者
Zhang, Yize [1 ]
Chen, Zailin [1 ,2 ,3 ,4 ]
Zhang, Chengjiang [1 ]
Ni, Shijun [1 ]
Cheng, Xianfeng [2 ,3 ]
Liu, Kexin [1 ]
机构
[1] Chengdu Univ Technol, Coll Earth & Planetary Sci, Chengdu 610059, Peoples R China
[2] Yunnan Educ Dept Hlth Geol Survey & Evaluat, Engn Ctr, Kunming 652501, Peoples R China
[3] Yunnan Land & Resources Vocat Coll, Kunming 652501, Peoples R China
[4] Chengdu Univ Technol, Appl Nucl Technol Geosci Key Lab Sichuan Prov, Chengdu 610059, Peoples R China
来源
OPEN GEOSCIENCES | 2024年 / 16卷 / 01期
关键词
Daduhe gold belt; mineralogy; geochemistry; mantle fluid model; prospecting potential; EASTERN NORTH CHINA; ORE-FORMING FLUIDS; OROGENIC GOLD; TECTONIC EVOLUTION; TIBETAN PLATEAU; YANGTZE BLOCK; GEOCHRONOLOGICAL CONSTRAINTS; TECTONOTHERMAL EVOLUTION; JIAODONG PENINSULA; METAL SOURCES;
D O I
10.1515/geo-2022-0736
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Geological characteristics, genetic model, and exploration implications in the Daduhe gold belt are studied. Three categories of gold deposits have been distinguished: "gold deposits in the basement (GDB)," "gold deposits in the cover layer (GDC)," and "gold deposits at the interface (GDI)." Among them, quartz vein type and quartz vein altered rock type are the main types of mineral deposits. The following features have been obtained: (1) inclusions of gold particles exist in pyrite, pyrrhotite, quartz, sellaite, and other sulfides; in fractures; or along cracks and grain margins. (2) The distribution curve of rare earth elements in pyrite and quartz indicates strong mineralization intensity in the GDB, (La/Sm)N fractionation characteristics, suggesting that pyrite may be more influenced by crustal materials and quartz by mantle materials. (3) The H-O and He-Ar isotopes manifested the ore-forming fluids derived from the mixing between crust and mantle. (4) The ranges of delta 34 S values of pyrite (-5.0 to 7.6 parts per thousand) are consistent with those of metasomatized mantle lithosphere. (5) The homogenization temperatures and salinity of all quartz inclusions are concentrated from 150 to 210 degrees C and 2.1-8.7 wt%, indicating a medium-low-temperature, low-salinity hydrothermal fluid. (6) The Daduhe orogenic gold deposits can be defined as epizonal subtypes. (7) The Daduhe gold deposits are medium-low temperature, low-salinity, and epizonal orogenic gold deposits, and fluid comes from a mixture of crust and mantle. In the future, efforts should be made to increase the exploration of deep gold deposits.
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页数:17
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