Published June 1983 | Version v1
Report

Mineralization typology

Creators

  • 1. Centre de Recherches Petrographiques et Geochimiques, 54 - Vandoeuvre-les-Nancy (France)
  • 2. Centre de Recherches sur la Geologie de l'Uranium, 54 - Vandoeuvre-les-Nancy (France)

Description

Uranium deposits spatially related to precambrian discordances present common mineralogical and geochemical features but also differences which give information on genesis. Uranium minerals described include uraninite, coffinite, brannerite, thucholite. Minerals found with uranium are briefly reviewed

Abstract (French)

Les gisements lies spatialement aux discordances proterozoiques presentent, d'un point de vue mineralogique et geochimique, des caracteres communs mais aussi des differences pouvant nous renseigner sur les conditions de genese. Les mineraux d'uranium comprennent les uraninites, coffinites, brannerites et tucholites. Les mineraux accompagnant l'uranium sont brievement passes en revue
Part of:
Uranium deposits spatially related to discordances

Additional details

Additional titles

Original title (French)
Typologie des mineralisations
Augmented title (English)
in uranium deposits

Publishing Information

ISBN
2-86783-000-1
Imprint Title
Uranium deposits spatially related to discordances
Imprint Pagination
380 p.
Journal Issue
No. 1
Series
Geol. Geochim. Uranium.
Journal Page Range
p. 305-315.
Report number
CREGU--1

Conference

Title
Seminar on uranium deposits spatially related to discordance.
Dates
26-28 Oct 1982.
Place
Nancy-Brabois (France).

INIS

Country of Publication
France
Country of Input or Organization
France
INIS RN
18060166
Subject category
S11: NUCLEAR FUEL CYCLE AND FUEL MATERIALS;
Resource subtype / Literary indicator
Conference
Descriptors DEI
GEOCHEMISTRY; MINERALOGY; URANIUM DEPOSITS; URANIUM MINERALS
Descriptors DEC
GEOLOGIC DEPOSITS; MATERIALS; MINERALS; RADIOACTIVE MATERIALS; RADIOACTIVE MINERALS

Optional Information

Notes
Imprint:Les gisements d'uranium lies spatialement aux discordances.;Comptes rendus du seminaire.