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Mesozoic magmatism and metallogeny in the Chizhou area, Middle-Lower Yangtze Valley, SE China: Constrained by petrochemistry, geochemistry and geochronology
被引:34
|作者:
Song, Guoxue
[1
,2
]
Qin, Kezhang
[1
]
Li, Guangming
[1
]
Evans, Noreen J.
[3
]
Li, Xianhua
[4
]
机构:
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
[3] Curtin Univ, John Laeter Ctr Isotope Res Appl Geol, Perth, WA 6845, Australia
[4] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
基金:
中国国家自然科学基金;
关键词:
Middle-Lower Yangtze Valley;
Chizhou;
Mesozoic;
Magmatism-mineralization;
Shangxi group;
Partial melting;
ZIRCON U-PB;
PLASMA-MASS SPECTROMETRY;
HF ISOTOPIC COMPOSITION;
W-MO DEPOSIT;
CONTINENTAL-CRUST;
EASTERN CHINA;
CHEMICAL-COMPOSITION;
VOLCANIC-ROCKS;
IGNEOUS ROCKS;
LOWER REACHES;
D O I:
10.1016/j.jseaes.2014.04.025
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
The Chizhou area, southeast China, hosts extensive W-Mo-Pb-Zn and Cu-Au deposits but remains relatively unstudied. A wide range of Mesozoic magmatic intrusives were analyzed (whole-rock geochemistry, Sr-Nd isotopes, zircon U-Pb dating, and zircon Lu-Hf isotopes) in order to elucidate their genesis, relationship to W-Mo-Pb-Zn-Cu-Au mineralization, and the tectonic setting of emplacement. Zircon U-Pb geochronology yielded a range of ages (147-110 Ma) encompassing three magmatic episodes; 147-135 Ma, 130-120 Ma, and 115-110 Ma. This work marks the first time the youngest episode has been identified. The oldest episode resulted in the formation of small granite porphyries, always associated with skarn-porphyry type W-Mo-Pb-Zn-Cu-Au deposits under an extensional setting. The 130-120 Ma and 115-110 Ma intrusives were the products of enhanced N-S extension with no associated mineralization. A comparative study reveals two types of magmatism-mineralization systems: acid magmatic rocks in the Chizhou area related to skarn-porphyry type W-Mo-Pb-Zn-Cu-Au deposits and intermediate-acid magmatic rocks in the Tongling area related to skarn-porphyry type Cu-Au-Fe-S deposits. Whole-rock Sr-Nd isotopes, zircon Lu-Hf isotopes, and inherited zircon U-Pb ages suggest that the lower crust and meso-neoproterozoic Shangxi group rocks were the main sources of magmatic rocks and related W-Mo-Pb-Zn-Cu-Au deposits. A genetic model for Mesozoic magmatism-skarn-porphyry type W-Mo-Pb-Zn-Cu-Au mineralization involves partial melting of the lower crust, mixing with the re-melted products of Meso-neoproterozoic Shangxi group rocks, and assimilation/fractional crystallization process. Results from this study suggest that there is great potential for the discovery of more and larger skarn-porphyry type W-Mo deposits in the transitional W-Mo-Pb-Zn metallogenic belt. (C) 2014 Elsevier Ltd. All rights reserved.
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页码:137 / 153
页数:17
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