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Supergene Uranyl Mineralization of the Rabejac Deposit, Lodève, France

机译:拉贝雅克矿床的超铀铀酰矿化作用,法国洛德夫

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The Rabejac uranium deposit that is located in the Lodève region, France, is the type locality for three uranyl minerals species (fontanite, seelite, and rabejacite). In addition, this deposit shows an extraordinary supergene uranyl mineralization characterized by the presence of many rare secondary uranyl species. In the present study, a mineralogical description as well as new chemical and crystallographic data are reported on (meta)zeunerite, (meta)nová?ekite, (meta)uranospinite, heinrichite, nová?ekite-I, arsenuranospathite, umohoite, calcurmolite, becquerelite, billietite, and liebigite. The chemical data indicate that the arsenate members of the autunite/meta-autunite group incorporate a significant amount of phosphorus. Moreover, the uranospinite samples usually exhibit high Mg content, thus moving toward the nová?ekite end-member composition. The refined unit-cell parameters for all of the investigated mineral species are in agreement with the previous data reported in the literature. Finally, a model describing the alteration of the primary uraninite and the formation of secondary uranyl minerals is proposed in agreement with the observed mineral assemblages.
机译:位于法国Lodève地区的Rabejac铀矿床是三种铀基矿物种类(方铁矿,Seelite和rabejacite)的典型产地。另外,该沉积物显示出异常的超基铀酰矿化,其特征是存在许多稀有的次要铀酰。在本研究中,据报道了以下矿物的矿物学描述以及新的化学和晶体学数据:(元)沸石,(元)新生沸石,(元)铀辉石,heinrichite,nováekite-I,亚砷酸钙石,umohoite,钙蒙脱石,珠光体,方铁矿和方铁矿。化学数据表明,金铁/金属-金铁矿组的砷酸盐成员掺入了大量的磷。此外,铀皂石样品通常表现出较高的Mg含量,因此会向新沸石端基成分移动。所有研究的矿物种类的精炼晶胞参数与文献中报道的先前数据一致。最后,与观察到的矿物组合相一致,提出了一个模型,该模型描述了初级铀尿石的蚀变和次级铀酰矿物的形成。

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