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Trace elemental signatures and mineral chemistry of clays associated with the alteration halos of the Paleoproterozoic U mineralization in Bijawars of the Sonrai Basin,Central India

跟踪元素的签名和在 Sonrai 盆的 Bijawars 与 Paleoproterozoic U 矿化作用的改变光圈联系的泥土的矿物质化学,中央印度

作     者:Surendra Kumar Jha Rashmi Sharma Jaya Prakash Shrivastava Surendra Kumar Jha;Rashmi Sharma;Jaya Prakash Shrivastava

作者机构:University of DelhiDelhiIndia Department of Cement TechnologyA.K.S.UniversitySatnaMPIndia 

出 版 物:《Acta Geochimica》 (地球化学学报(英文))

年 卷 期:2020年第39卷第3期

页      面:365-386页

核心收录:

学科分类:081803[工学-地质工程] 0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 08[工学] 0818[工学-地质资源与地质工程] 

基  金:JPS acknowledges Delhi University for financial support towards this work in the form of R&D Project Grant(No.DRCH/R&D/2012-2013/4155) 

主  题:Bijawars Sonrai basin Clays REE patterns Uranium mineralization 

摘      要:Paleoproterozoic Bijawars of the Sonrai basin consists of(a) Sonrai(mostly carbonate carbonaceous shale and phosphatic breccia) and(b) Solda Formations(commonly chloritic and ferruginous shale) with well-developed clay-organo-rich facies,often marked with hydrothermal *** studies revealed abundance order of kaolinite chlorite illite smectite;and kaolinite illite chlorite in clay(0.2-2.0 μm) fractions separated from the Sonrai and Solda Formations,*** understand atomic substitutions and trace elemental concentrations,clay minerals were analyzed by fusion ICPMS and *** normalized data plots show U,Th,Rb,Ba,Pb Sr,and large-ion lithophiles enrichment,whereas,Bandai sandstone and Rohini carbonate clays show HREE enrichment with asymmetrical patterns,similar to those reported from the well-established McArthur River,Cigar Lake,and Sue UTUD of *** Rohni carbonate,chondrite-normalized REE data plots revealed M shape REE patterns,ascribed to Gd-Tb-Dy-Ho tetrad effect and anomalous Y,Zr,and Hf *** to HREE incorporation in the clay inter-layers,linear and flattened REE trends were *** REE patterns associated with the highly altered chlorite and illite represent negative Eu anomaly related to the dilational nature of the uraninite structure and is suggestive of anoxic conditions.

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