2005 | OriginalPaper | Buchkapitel
Late Mesozoic-Cenozoic tectono-sedimentary evolution and sandstone-hosted uranium mineralization of the Erlian basin
verfasst von : Sanyuan Wei, Mingkuan Qiu, Yuexiang Li, Zhongbo He, Anping Chen, Kefeng Shen
Erschienen in: Mineral Deposit Research: Meeting the Global Challenge
Verlag: Springer Berlin Heidelberg
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The tectono-sedimentary evolution of the Erlian basin can be divided into 3 stages: continental extension and down-faulting, transformation of down-faulting to down-warping, weak compression and differential uplifting-subsidence. Clastic rocks developed in the transformation stage of down-faulting to down-warping are the main ore-hosting beds. The stages of weak compression and differential uplifting-subsidence provide conditions for uranium mineralization. Uranium metallogenic conditions have been analyzed, and a metallogenic model of uranium deposits discovered recently in the Baiyiwula area are summarized.