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- W2351901997 abstract "The Nanling area in northern Guangdong Province is important for its granitic uranium deposits.The characteristics of the structures and ESR ages of the hydrothermal quartz show that the ore field underwent three stages of structural deformation in Cenozoic:(65.5~55.0Ma) differential uplifting of land mass and colossal faults movements;Ⅱ(40.3~20.0Ma) intermittent faulting and uplifting,Ⅲ(20.0~2.2Ma) frequent small scale hydrothermal activities.ESR ages of hydrothermal quartz and U-Pb ages of pitchblender from 331,335,336 uranium deposits demonstrate that the U mineralization took place no later than 60Ma±,which is consistent with the first stage deformation.The second and third stage deformation resulted in uplifting and frequent faulting.The NNE,NEE and the EW-trending structures exhibit chess-board pattern in horizontal and graben-like pattern vertically.The structures aggravated weathering,leaching and denudation processes,and finally destroyed the pre-exist metallogenic environment.Thus,study of the Cenozoic tectonic evolution may contribute to the understanding of the tectonic controls on the uranium ore forming processes." @default.
- W2351901997 created "2016-06-24" @default.
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- W2351901997 date "2011-01-01" @default.
- W2351901997 modified "2023-09-25" @default.
- W2351901997 title "Cenozoic Tectonic Evolution and its Influence on Uranium Ore-forming Processes in the Xiazhuang Ore Field,Northern Guangdong Province" @default.
- W2351901997 hasPublicationYear "2011" @default.
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