原文服务方: 地球化学学报(英文)       
摘要:
Some Au deposits in southern Anhui Province have recently been found to be closely associated with Late Mesozoic intrusions. Typical examples include the Huashan Au (Sb) deposit and Au deposits at Zhaojialing, Wuxi, and Liaojia. In order to understand the mechanisms that led the formation of these Au deposits, we make detailed reviews on the geological characteristics of these Au deposits. Specifically, we present new LA-ICP-MS zircon U-Pb dating, along with elemental and Hf isotopic data from the Huashan Au (Sb) deposit. Our data suggests that the Huashan ore-related intrusions were emplaced during the Late Jurassic and Early Cretaceous periods (144-148 Ma). They are characterized by arc-magma features and high oxygen fugacity and are rich in inherited zircons. Zircon U-Pb ages and Lu-Hf isotopes from intrusions suggest that Proterozoic juvenile lithosphere is the main source of these intrusions. The regional geological history implies that lithosphere beneath southern Anhui was produced during a Proterozoic subduction and was fertilized with Au (Cu) in the process. Integrated with the results of previous studies, we inferred that Late Mesozoic intrusions formed by the remelting of the lithosphere could provide the metal endowment for the Au-rich deposits in southern Anhui.
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篇名 Geochemistry and geochronology of Late Jurassic and Early Cretaceous intrusions related to some Au (
来源期刊 学科 地球科学
关键词 Yanshannian magmatism Subduction-modified lithosphere Au (Sb) deposits Southern Anhui South China
年,卷(期) 2022,(3) 所属期刊栏目
研究方向 页码范围 360-383
页数 23页 分类号
字数 语种 英文
DOI 10.1007/s11631-018-0270-y
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Yanshannian magmatism
Subduction-modified lithosphere
Au (Sb) deposits
Southern Anhui
South China
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地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
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230
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