Published December 1996 | Version v1
Journal article Metadata-only

New interpretation of the dominant ore-controlling factor of the uranium ore field No. 322

Creators

  • 1. Central-South Bureau of Uranicem Geology CNNC, Changsha, HN (China)

Description

The NE-trending fault structures in ore field NO. 322 are characterized by compress-shearing, left-Lateral left-slipping, having an obvious control over the Localisation of the ore field No. 322, and are the dominant ore-controlling factor of the ore field NO.322. Resulting from the sinistral displacement of the NE-trending fault, there is a pull-apart basin in the Feng Zhou area. The formation and evolution of the NE-trending fault zone and the Feng Zhou basin control the formation of uranium deposits of ore field No. 322

Additional details

Publishing Information

Journal Title
Journal of East China Geological Institute
Journal Volume
19
Journal Issue
4
Journal Page Range
p. 355-362.
ISSN
1000-2251
CODEN
HUDXEZ

INIS

Country of Publication
China
Country of Input or Organization
China
INIS RN
28046644
Subject category
S11: NUCLEAR FUEL CYCLE AND FUEL MATERIALS;
Descriptors DEI
CHINA; GEOCHEMISTRY; GEOLOGIC FRACTURES; GRANITES; MINERALIZATION; PRECIPITATION; RADIONUCLIDE MIGRATION; URANIUM; URANIUM DEPOSITS
Descriptors DEC
ACTINIDES; ASIA; ELEMENTS; ENVIRONMENTAL TRANSPORT; GEOLOGIC DEPOSITS; GEOLOGIC STRUCTURES; IGNEOUS ROCKS; MASS TRANSFER; METALS; PLUTONIC ROCKS; ROCKS; SEPARATION PROCESSES