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.
引用
收藏
页码:137 / 153
页数:17
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