4.7 Article

Episodic Nb-Ta mineralisation in South China: Constraints from in situ LA-ICP-MS columbite-tantalite U-Pb dating

Journal

ORE GEOLOGY REVIEWS
Volume 105, Issue -, Pages 71-85

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.oregeorev.2018.11.023

Keywords

Columbite-tantalite; LA-ICP-MS U-Pb dating; Episodic mineralisation; South China

Funding

  1. Natural Science Foundation of China [41672065, 41230315, 41572058, 41572045]
  2. National Key R&D Program of China [2016YFC0600203]
  3. Fundamental Research Funds for the Central Universities, China [020614380057]

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South China hosts many Nb-Ta deposits that show evidence for episodic mineralization, which were generated during the emplacement of composite granites. To constrain the spatio-temporal distribution of Nb-Ta mineralisation in the region and to identify future targets for mineral exploration, we used in situ laser ablation inductively coupled plasma-mass spectroscopy to date 23 columbite-tantalite group mineral (CGM) samples from 14 Nb-Ta deposits. Our CGM U-Pb data, supplemented by previous results, reveal five distinct Nb-Ta mineralisation events in South China as follows: (1) Late Silurian-Middle Devonian (ca. 424-391 Ma; e.g., the Xigang and Nanping deposits in eastern Jiangxi and western Fujian Provinces); (2) Triassic (ca. 248-204 Ma; e.g., the Houxi, Cunxin, Dongtounan, Shenkeng, Limu and Gaoling deposits in western Guangdong Province and northeastern Guangxi Zhuang Autonomous Region; (3) Late Jurassic (ca. 160-150 Ma; e.g., the Gedongping, Yichun, Laiziling, Jianfengling and Jinzhulong deposits in Guangxi, Jiangxi and Hunan Provinces); (4) Early Cretaceous (ca. 130 Ma; e.g., the Huangshan and Songshugang deposits in northeastern Jiangxi province); and (5) Late Cretaceous (ca. 90 Ma; e.g., the Jiepailing deposit, located along the boundary between Hunan and Jiangxi Provinces). We show that Nb-Ta mineralisation in South China was controlled by multiple tectono-magmatic events. Our CGM samples yielded Caledonian (ca. 424-391 Ma), early Indosinian (ca. 248 Ma) and late Yanshanian (ca. 130 Ma) ages, indicating that Nb-Ta mineralisation was abundant during these times and should form the focus for future studies of mineralisation in the region. Early Triassic granite in the Guangning Nb-Ta metallogenic district in western Guangdong Province, Indosinian and early Yanshannian granites in the Miao'ershan-Yuechengling batholith in northeastern Guangxi, and the Late Cretaceous Lingshan batholith in northern Jiangxi Province are identified as targets for future Nb-Ta exploration.

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