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The uranium bearing shale ore-body at St-Hippolyte (Haut-Rhin). An example of research with statistical methods; Le gisement des schistes uraniferes de St-Hippolyte (Haut-Rhin). Exemple d'etude par calculs statistiques

Abstract

The uranium bearing shale ore-body at St-Hippolyte was mainly proved by drillings, the results of which were studied through statistical methods. The author gives an account of his conclusions regarding the distribution of mineralization, its origin and, the estimate of reserves. The uranium mineralization is irregularly distributed in shales. On a vertical line, levels could be singled out: they are similar, as far as lithology is concerned, but each of them is characterized by a grade-population, according to a lognormal distribution. Horizontally, a connection is noted between grades and the overlying barren sandstone bed. These considerations, as well as a statistical study of U/Ra ratio, induced the author to consider that the mineralization of the richest level has an hydrothermal origin. It is only through an uranium diffusion from that level that the others are mineralized. The uranium which is contained in poorest beds has a syn-genetic origin. Furthermore, statistical methods bring us to an evaluation of reserves. In such a case, the evaluation is equivalent to the ore obtained by common arithmetical methods. Moreover, we are able to state precisely the upper and lower limits where a true tonnage or a true grade could be given with a definite  More>>
Authors:
Carlier, A [1] 
  1. Commissariat a l'Energie Atomique, Saclay (France). Centre d'Etudes Nucleaires
Publication Date:
Jul 01, 1958
Product Type:
Technical Report
Report Number:
CEA-R-1033
Subject:
11 NUCLEAR FUEL CYCLE AND FUEL MATERIALS; ABUNDANCE; COMPARATIVE EVALUATIONS; CORRELATIONS; DATA COVARIANCES; FRANCE; HYDROTHERMAL STAGE; INVENTORIES; LITHOLOGY; MINERALIZATION; ORE COMPOSITION; PROBABILISTIC ESTIMATION; RADON; RESOURCE ASSESSMENT; SCHISTS; SITE CHARACTERIZATION; SPATIAL DISTRIBUTION; STRATIGRAPHY; URANIUM DEPOSITS; URANIUM RESERVES
OSTI ID:
20912749
Research Organizations:
CEA Saclay, 91 - Gif-sur-Yvette (France)
Country of Origin:
France
Language:
French
Other Identifying Numbers:
TRN: FR07R1033073925
Availability:
Available from INIS in electronic form
Submitting Site:
FRN
Size:
22 pages
Announcement Date:
Sep 22, 2007

Citation Formats

Carlier, A. The uranium bearing shale ore-body at St-Hippolyte (Haut-Rhin). An example of research with statistical methods; Le gisement des schistes uraniferes de St-Hippolyte (Haut-Rhin). Exemple d'etude par calculs statistiques. France: N. p., 1958. Web.
Carlier, A. The uranium bearing shale ore-body at St-Hippolyte (Haut-Rhin). An example of research with statistical methods; Le gisement des schistes uraniferes de St-Hippolyte (Haut-Rhin). Exemple d'etude par calculs statistiques. France.
Carlier, A. 1958. "The uranium bearing shale ore-body at St-Hippolyte (Haut-Rhin). An example of research with statistical methods; Le gisement des schistes uraniferes de St-Hippolyte (Haut-Rhin). Exemple d'etude par calculs statistiques." France.
@misc{etde_20912749,
title = {The uranium bearing shale ore-body at St-Hippolyte (Haut-Rhin). An example of research with statistical methods; Le gisement des schistes uraniferes de St-Hippolyte (Haut-Rhin). Exemple d'etude par calculs statistiques}
author = {Carlier, A}
abstractNote = {The uranium bearing shale ore-body at St-Hippolyte was mainly proved by drillings, the results of which were studied through statistical methods. The author gives an account of his conclusions regarding the distribution of mineralization, its origin and, the estimate of reserves. The uranium mineralization is irregularly distributed in shales. On a vertical line, levels could be singled out: they are similar, as far as lithology is concerned, but each of them is characterized by a grade-population, according to a lognormal distribution. Horizontally, a connection is noted between grades and the overlying barren sandstone bed. These considerations, as well as a statistical study of U/Ra ratio, induced the author to consider that the mineralization of the richest level has an hydrothermal origin. It is only through an uranium diffusion from that level that the others are mineralized. The uranium which is contained in poorest beds has a syn-genetic origin. Furthermore, statistical methods bring us to an evaluation of reserves. In such a case, the evaluation is equivalent to the ore obtained by common arithmetical methods. Moreover, we are able to state precisely the upper and lower limits where a true tonnage or a true grade could be given with a definite value of statistical certainty. Then the author has been able to study the separation of reserves in grade-groups and to foresee the effect of sorting in connection with the lower possible grade and with extraction units (wagons, lorries, etc...), on which the sorting will be done. To conclude, the author indicates the value of both classical and statistical methods. These two techniques are completing each other and they solve different problems. (author) [French] Le gisement des schistes uraniferes de St-Hippolyte a ete reconnu essentiellement par sondages, dont les resultats ont ete etudies par les methodes du calcul statistique. L'auteur expose les conclusions auxquelles il a ete amene et qui concernent: la repartition de la mineralisation, son origine et l'evaluation des reserves. La mineralisation est inegalement repartie dans les schistes. Dans le sens vertical, on distingue plusieurs niveaux, lithologiquement semblables, mais caracterises chacun par une population de teneurs qui obeit a la loi lognormale. Dans le sens horizontal, on note une relation entre les teneurs et la couverture greseuse sterile. Ces considerations, ainsi que l'etude statistique du rapport U/Ra, conduisent l'auteur a considerer que la mineralisation du niveau le plus riche est d'origine hydrothermale; les autres niveaux ne sont mineralises que par une diffusion de l'uranium, a partir du precedent. L'uranium contenu dans les couches les plus pauvres est d'origine syngenetique. Les calculs statistiques conduisent de plus a une estimation des reserves du gisement. Dans le cas considere, cette estimation est equivalente a celle que l'on obtient par la methode arithmetique classique. Mais on arrive en outre a preciser les limites superieures et inferieures entre lesquelles se situent, soit le tonnage vrai, soit la teneur vraie, a un niveau de certitude donne. Enfin, l'auteur a pu ainsi etudier la decomposition des reserves en tranches de teneurs, et prevoir l'effet du triage, en fonction de la teneur de coupure adoptee et des unites d'extraction (berlines, camions, etc) sur lesquelles sera opere le triage. L'auteur montre en conclusion, l'interet qui s'attache respectivement a la methode classique d'evaluation et a la methode statistique. Ces deux methodes se completent et repondent a des preoccupations differentes. (auteur)}
place = {France}
year = {1958}
month = {Jul}
}