Published June 2013
| Version v1
Journal article
Ore-forming fluid features and metallogenic model of uranium deposits in Zhuguangshan ore field
Creators
- 1. Hunan Province Nuclear Geological Bureau, Changsha (China)
- 2. CNNC Key Laboratory of Uranium Resources Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beijing (China)
Description
Based on the analysis of geological backgrounds in Zhuguangshan ore field, this paper discussed the metallogenic character and ore-forming fluid features of the uranium deposits and summarized the metallogenic model. Precambrian basement, Indo-Chinese and Yanshan epoch granite mass which is the uranium sources, were altered and extracted by upper mantle hydrothermal fluid and generated the ore-forming fluid. Mineralization is controlled by Late Mesozoic outstretch structure and deep focus hydrothermal fluid. 3 metallogenetic types were classified in this ore field: crack alteration granite veinlet disseminations type, silicate crack granite vein type and dynamic breccia vein type. (authors)
Additional details
Publishing Information
- Journal Title
- World Nuclear Geoscience
- Journal Volume
- 30
- Journal Issue
- 2
- Journal Page Range
- p. 63-69, 78
- ISSN
- 1672-0636
INIS
- Country of Publication
- China
- Country of Input or Organization
- China
- INIS RN
- 48045361
- Subject category
- S11: NUCLEAR FUEL CYCLE AND FUEL MATERIALS; S58: GEOSCIENCES;
- Descriptors DEI
- CRACKS; FLUIDS; GEOCHEMISTRY; GRANITES; MINERALIZATION; URANIUM; URANIUM DEPOSITS
- Descriptors DEC
- ACTINIDES; CHEMISTRY; ELEMENTS; GEOLOGIC DEPOSITS; IGNEOUS ROCKS; METALS; MINERAL RESOURCES; PLUTONIC ROCKS; RESOURCES; ROCKS
Optional Information
- Notes
- 1 fig., 8 refs.