马哈拉施特拉邦南兰德地区东南部放射性花岗岩和硅质碎裂岩流体包裹体研究:铀矿化意义

R. Banerjee, K. Shivkumar, T. Thomas, Jugina Thomas, M. S. Pandian
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引用次数: 0

摘要

在马哈拉施特拉邦南德地区东南部的thadiisaoli - khatgaon和Shahpur-Sujayatpur地区,发现了放射性花岗岩类和硅质碎裂岩,并记录了异常的放射性元素含量(花岗岩:U3O8高达1%,ThO2高达0.20%;Cherty碎裂岩U3O8含量高达0.11%,ThO2含量<0.005%),并富集微量元素和稀有金属及稀土元素浓度(Nb:可达146ppm, Y:可达226ppm, Zr:可达559ppm,总REE:可达2010ppm)。矿化花岗岩类受丰富的伟晶岩/石英长石、石英和绿长岩脉系影响,主要局限于NE-SW和NNE-SSW断裂/剪切带。放射性相以离散的铀/钍矿矿物(铀矿、β-铀矿和钍矿)和高含量的抗性矿物(磷灰石、锆石、allanite、榍石、铈矿、独居石和钛铁矿)为代表。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fluid inclusion study of radioactive granitoids and cherty cataclasite in the southeastern part of Nanded district, Maharashtra: implications for Uranium mineralisation
Radioactive granitoids and cherty cataclasites are delineated in Thadisaoli–Khatgaon and Shahpur–Sujayatpur sectors in southeastern part of Nanded district, Maharashtra, which have recorded anomalous radioelemental contents (Granites: upto 1% U3O8 and 0.20% ThO2; Cherty cataclasites upto 0.11% U3O8 and <0.005% ThO2) and enrichment in trace element and rare metal and rare earth element concentration (Nb: upto 146ppm, Y: upto 226ppm, Zr: upto 559ppm and total REE: upto 2010ppm). The mineralised granitoids are affected by profuse pegmatitic/quartzo-feldspathic, quartz and epidote venations and mainly confined along the NE–SW and NNE–SSW faults/shear zones. Radioactive phases are represented by discrete uranium/thorium ore minerals (uraninite, β-uranophane and thorite) and high content of resistates viz., apatite, zircon, allanite, sphene, cerianite, monazite and ilmenite.
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