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Evolution of fluid types at the Rozna uranium deposit, Czech Republic: Stable isotope and fluid inclusion study

机译：瑞萨铀矿床流体类型的演变，捷克共和国：稳定同位素和流体包容性研究

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Hydrothermal mineralization of the Rozna uranium deposit, located in the high-grade metamorphosed Moldanubian Unit in the eastern part of the Bohemian Massif, was formed during several successive stages of fluid flow through a regional shear/fault zone. Individual stages are characterized by distinct fluid types and different physical and chemical conditions, and were significantly separated in time.

机译：罗扎纳铀矿床的水热矿化，位于波希米亚群体东部的高档变质摩兰达邦单元，在通过区域剪切/断层区的几个流体流动的连续阶段形成。单个阶段的特征在于不同的流体类型和不同的物理和化学条件，并及时显着分离。

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《Biennial SGA-SEG meeting》|2001年||共5页
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P. Dob; D. Holeczy; A. Hajek; M. Pudilova; B. Kribek; P. Dobes; K. Zak;
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Evolution of fluid types at the Rozna uranium deposit, Czech Republic: Stable isotope and fluid inclusion study

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