You need JavaScript to view this

Uranium mineralization of migmatite in southern China

Journal Article:

Abstract

The uranium mineralization occurs in migmatite in the form of disseminated uraninite is a new type found in southern China. According to the forms of uraninite existence in orebodies, it can be divided into primary and reworked subtypes. The principal uranium mineral in the deposits of primary subtype is uraninite, but those in reworked subtype are pitchblende and relict uraninite. The formation of uranium mineralization is considered as a result of remobilization, migration and local concentration caused by preferential melting of the uranium-rich strata.
Authors:
Publication Date:
Sep 01, 1987
Product Type:
Journal Article
Reference Number:
AIX-19-087889; EDB-88-160268
Resource Relation:
Journal Name: Uranium Geol.; (China); Journal Volume: 3:5
Subject:
11 NUCLEAR FUEL CYCLE AND FUEL MATERIALS; URANIUM ORES; METAMORPHIC ROCKS; MINERALIZATION; CHINA; METAMORPHISM; PITCHBLENDE; URANINITES; URANIUM; ACTINIDES; ASIA; ELEMENTS; MATERIALS; METALS; MINERALS; ORES; RADIOACTIVE MATERIALS; RADIOACTIVE MINERALS; ROCKS; URANIUM MINERALS; 050100* - Nuclear Fuels- Reserves, Exploration, & Mining
OSTI ID:
7120975
Country of Origin:
China
Language:
Chinese
Other Identifying Numbers:
Journal ID: CODEN: YODIE
Submitting Site:
INIS
Size:
Pages: 276-280
Announcement Date:

Journal Article:

Citation Formats

Feng, Mingyue. Uranium mineralization of migmatite in southern China. China: N. p., 1987. Web.
Feng, Mingyue. Uranium mineralization of migmatite in southern China. China.
Feng, Mingyue. 1987. "Uranium mineralization of migmatite in southern China." China.
@misc{etde_7120975,
title = {Uranium mineralization of migmatite in southern China}
author = {Feng, Mingyue}
abstractNote = {The uranium mineralization occurs in migmatite in the form of disseminated uraninite is a new type found in southern China. According to the forms of uraninite existence in orebodies, it can be divided into primary and reworked subtypes. The principal uranium mineral in the deposits of primary subtype is uraninite, but those in reworked subtype are pitchblende and relict uraninite. The formation of uranium mineralization is considered as a result of remobilization, migration and local concentration caused by preferential melting of the uranium-rich strata.}
journal = {Uranium Geol.; (China)}
volume = {3:5}
journal type = {AC}
place = {China}
year = {1987}
month = {Sep}
}