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.
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 = []
volume = {3:5}
journal type = {AC}
place = {China}
year = {1987}
month = {Sep}
}
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 = []
volume = {3:5}
journal type = {AC}
place = {China}
year = {1987}
month = {Sep}
}