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Geology, Geochronology, and Hf Isotopic Composition of the Pha Lek Fe Deposit, Northern Laos: Implications for Early Permian Subduction-Related Skarn Fe Mineralization in the Truong Son Belt
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  • 英文篇名:Geology, Geochronology, and Hf Isotopic Composition of the Pha Lek Fe Deposit, Northern Laos: Implications for Early Permian Subduction-Related Skarn Fe Mineralization in the Truong Son Belt
  • 作者:Lin ; Hou ; Shusheng ; Liu ; Linnan ; Guo ; Fuhao ; Xiong ; Chao ; Li ; Meifeng ; Shi ; Qiming ; Zhang ; Siwei ; Xu ; Songyang ; Wu
  • 英文作者:Lin Hou;Shusheng Liu;Linnan Guo;Fuhao Xiong;Chao Li;Meifeng Shi;Qiming Zhang;Siwei Xu;Songyang Wu;Chengdu Center,China Geological Survey;Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Land and Resources, Chengdu University of Technology;National Research Center of Geoanalysis, Chinese Academy of Geological Science;China University of Geosciences;
  • 英文关键词:Truong Son belt;;Pha Lek Fe deposit;;granitic intrusions;;geochronology;;Hf isotopic composition
  • 中文刊名:ZDDY
  • 英文刊名:地球科学学刊(英文版)
  • 机构:Chengdu Center,China Geological Survey;Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Land and Resources, Chengdu University of Technology;National Research Center of Geoanalysis, Chinese Academy of Geological Science;China University of Geosciences;
  • 出版日期:2019-02-01
  • 出版单位:Journal of Earth Science
  • 年:2019
  • 期:v.30
  • 基金:supported financially by the National Natural Science Foundation of China (Nos. 41402074 and 41502074);; Applied Fundamental Research Funding of Sichuan Province, China (No. 2015JY0055);; the National Geological Survey Foundation of China (No. 121201010000150013)
  • 语种:英文;
  • 页:ZDDY201901009
  • 页数:12
  • CN:01
  • ISSN:42-1788/P
  • 分类号:117-128
摘要
The Truong Son metallogenic belt in central Laos and Vietnam is an important Fe-Cu-Sn-Au polymetallic ore district. The Pha Lek Fe deposit is closely related to Late Carboniferous– Early Permian I-type granitic magmatism, and contains >50 Mt @ 45% to 50% of Fe ore. Ore minerals occur mainly as magnetite and hematite in the skarn alteration zone between a granitic pluton and metamorphosed Middle–Upper Devonian carbonates. The granitic pluton comprises granodiorite and granite, with zircon U-Pb dating indicating synchronous emplacement at 288.2±1.3 and 284.9±1.2 Ma, respectively. Zircons from these granitoids have ε_(Hf)(t) values of 2.9–11.2 and relatively young TDM2 ages(<1.0 Ga), indicating an origin by partial melting of depleted mafic crust or magma mixing. Previous studies have shown that these granitoids have high Y, Yb, and K_2O contents, and low Sr and Na_2O contents, which are interpreted as the melting of mafic continental crust. Pyrite of the main mineralization stage yields an ~(187)Re/~(188)Os-~(187)Os/~(188)Os isochron age of 287±17 Ma, indicating that mineralization is associated with Pha Lek granitic magmatism. A Late Carboniferous–Early Permian subduction-related skarn-type Fe mineralization model is proposed for the Pha Lek deposit. More evidence is needed to verify a hypothesis of volcanic overprinting during Late Triassic post-collisional extension.
        The Truong Son metallogenic belt in central Laos and Vietnam is an important Fe-Cu-Sn-Au polymetallic ore district. The Pha Lek Fe deposit is closely related to Late Carboniferous– Early Permian I-type granitic magmatism, and contains >50 Mt @ 45% to 50% of Fe ore. Ore minerals occur mainly as magnetite and hematite in the skarn alteration zone between a granitic pluton and metamorphosed Middle–Upper Devonian carbonates. The granitic pluton comprises granodiorite and granite, with zircon U-Pb dating indicating synchronous emplacement at 288.2±1.3 and 284.9±1.2 Ma, respectively. Zircons from these granitoids have ε_(Hf)(t) values of 2.9–11.2 and relatively young TDM2 ages(<1.0 Ga), indicating an origin by partial melting of depleted mafic crust or magma mixing. Previous studies have shown that these granitoids have high Y, Yb, and K_2O contents, and low Sr and Na_2O contents, which are interpreted as the melting of mafic continental crust. Pyrite of the main mineralization stage yields an ~(187)Re/~(188)Os-~(187)Os/~(188)Os isochron age of 287±17 Ma, indicating that mineralization is associated with Pha Lek granitic magmatism. A Late Carboniferous–Early Permian subduction-related skarn-type Fe mineralization model is proposed for the Pha Lek deposit. More evidence is needed to verify a hypothesis of volcanic overprinting during Late Triassic post-collisional extension.
引文
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