The metallogenic characteristics and exploring ore potential of the gold deposits in eastern Liaoning Province
文献类型:期刊论文
作者 | Zeng QingDong1,4,5; Chen RenYi3; Yang JinHui1,2,4; Sun GuoTao1,4,5; Yu Bing1,4,5; Wang Yongbin1,4,5; Chen PeiWen1,4,5 |
刊名 | ACTA PETROLOGICA SINICA
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出版日期 | 2019 |
卷号 | 35期号:7页码:1939-1963 |
关键词 | Hydrothermal gold deposit Ore-forming system Ore-concentrated area Mesozoic Eastern Liaoning Province |
ISSN号 | 1000-0569 |
DOI | 10.18654/1000-0569/2019.07.01 |
英文摘要 | The eastern Liaoning Province is one of the most important Au ore-concentrated areas in China. The Mesozoic tectonic and magmatic activities developed in eastern Liaoning Province accompanied with the intense gold mineralization. According to the time-space distributions and metallogenic characteristics of the gold deposits, the eastern Liaoning Province can be divided into three gold ore-concentrated districts: the Qingchengzi, the Wulong and the Maoliang districts. Gold deposits includes two gold mineralization types: quartz vein type and altered rock type. The quartz vein type gold deposits are controlled by the high-angle fault system, and the altered rock type gold deposits are controlled by the low-angle fault system. The ore-forming epochs of the gold mineralization in eastern Liaoning Province are major Early Cretaceous with minor Early Jurassic. Combing with the H-O isotopes, ore-forming fluids and geological studies, we think that: (1) the gold mineralization is related to the Mesozoic magmatic activities, and is characterized by the strong silicification and sericitization; (2) the gold deposits belong to the magmatic hydrothermal gold deposit; and (3) the filling and mixing might be the major depositional mechanism of the gold deposits. The gold hydrothermal ore-forming system of the eastern Liaoning Province is divided into two sub-ore-forming systems by the occurrence environment and features of the gold deposits: the gold ore-forming system hosted in Mesozoic granitoids (the Wulong type) and the gold ore-forming system hosted in Paleoproterozoic metamorphic rocks (the Qingchengzi type and Maoling type). By integrating the progress of the prospecting and recent studies, we set up the geological model of prospecting and prediction for gold deposits in Liaodong area, and proposed that eastern Liaodong area has the similar gold ore-forming conditions with the Jiaodong area, and therefore, the eastern Liaodong area also has huge metallogenic potentiality. The studied works has guiding significance for the regional mineral prospecting. |
WOS关键词 | NORTH CHINA CRATON ; ZIRCON U-PB ; LIAODONG PENINSULA ; JI BELT ; SILVER DEPOSIT ; GEOCHRONOLOGICAL CONSTRAINTS ; TECTONIC IMPLICATIONS ; ISOTOPE GEOCHEMISTRY ; CRUSTAL EVOLUTION ; FLUID INCLUSIONS |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000491151100001 |
出版者 | SCIENCE PRESS |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/93915] ![]() |
专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 地质与地球物理研究所_岩石圈演化国家重点实验室 |
通讯作者 | Zeng QingDong |
作者单位 | 1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 3.Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China 4.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China 5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Zeng QingDong,Chen RenYi,Yang JinHui,et al. The metallogenic characteristics and exploring ore potential of the gold deposits in eastern Liaoning Province[J]. ACTA PETROLOGICA SINICA,2019,35(7):1939-1963. |
APA | Zeng QingDong.,Chen RenYi.,Yang JinHui.,Sun GuoTao.,Yu Bing.,...&Chen PeiWen.(2019).The metallogenic characteristics and exploring ore potential of the gold deposits in eastern Liaoning Province.ACTA PETROLOGICA SINICA,35(7),1939-1963. |
MLA | Zeng QingDong,et al."The metallogenic characteristics and exploring ore potential of the gold deposits in eastern Liaoning Province".ACTA PETROLOGICA SINICA 35.7(2019):1939-1963. |
入库方式: OAI收割
来源:地质与地球物理研究所
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