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| Citation: | Zhang Yiyang, Zhong Fujun, Pan Jiayong, Xia Fei, Qi Jiaming, Li Haidong, Liu Wenquan, 2022. Petrogenesis and Its Relationship with Uranium Mineralization of Diabase in Huangsha Uranium Ore-Field, South Jiangxi Province. Earth Science, 47(1): 206-223. doi: 10.3799/dqkx.2021.132
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The diabase dikes in the Huangsha U ore-field of South Jiangxi Province have close spatial relationship with U mineralization. The petrography, major element, trace element and Sr-Nd-Pb isotope analysis of diabase were carried out. The diabase is geochemically characterized by low SiO2, MgO and alkaline, Na2O > K2O, enrichment of large ion lithophile elements (Sr, K, Rb, Ba), no fractionation in LREE and HREE (LREE/HREE=2.81-2.97), weak Eu negative anomaly(δEu=0.95-0.98), typical Dupal anomaly Pb isotopic, high (87Sr/86Sr)i(0.704 93-0.706 58) and low εNd(t) (3.98-4.84), suggesting that the diabase belongs to continental tholeiite series, the magmatic source was the relatively enriched mantle changed by the metasomatism fluid originated from the subduction zone of Pacific Ocean Plate, formed under the large scale lithosphere thining tectonic background. The gaps between diagenetic ages of diabase (140 Ma) and uranium mineralization ages (100 Ma, 63-76 Ma) are significantly large. It is considered that diabase provides a favorable reductive agent for pitchblende precipitation. Comparing the diabase in the Zhuguang-Xiazhuang ore-field, there are many similarities in origin and ore-controlling rules. In Huangsha U ore-field, there are favorable geological conditions for U mineralizaiton and great metallogenetic potentiality. The exploration for U deposit in the future should focus on the intersection type U mineralization and the intersection of NWW-trending basic dikes and NE-trending fracture zone.
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