Abstract
The lithological and geochemical conditions relative to the ''Senonian'' phosphatic chalks are relatively simple in the Basins of Mons (Belgium) and of Picardy (France). Their characteristics permit us to study chiefly the uranium-phosphate relation. It appears a very good linear correlation between the phosphate and the uranium. The coefficient U/P/sub 2/O/sub 5/ remains a constant from the bottom to the top of the same section, but changes in space for synchronic formations (lateral variation of geochemical facies) and in time for two separated basins.
Citation Formats
Quinif, Y, Charlet, J M, Dupuis, C, and Robaszynski, F.
Uranium-phosphate relationship in phosphated chalks of the Mons and Picardie Bassins.
France: N. p.,
1981.
Web.
Quinif, Y, Charlet, J M, Dupuis, C, & Robaszynski, F.
Uranium-phosphate relationship in phosphated chalks of the Mons and Picardie Bassins.
France.
Quinif, Y, Charlet, J M, Dupuis, C, and Robaszynski, F.
1981.
"Uranium-phosphate relationship in phosphated chalks of the Mons and Picardie Bassins."
France.
@misc{etde_5262759,
title = {Uranium-phosphate relationship in phosphated chalks of the Mons and Picardie Bassins}
author = {Quinif, Y, Charlet, J M, Dupuis, C, and Robaszynski, F}
abstractNote = {The lithological and geochemical conditions relative to the ''Senonian'' phosphatic chalks are relatively simple in the Basins of Mons (Belgium) and of Picardy (France). Their characteristics permit us to study chiefly the uranium-phosphate relation. It appears a very good linear correlation between the phosphate and the uranium. The coefficient U/P/sub 2/O/sub 5/ remains a constant from the bottom to the top of the same section, but changes in space for synchronic formations (lateral variation of geochemical facies) and in time for two separated basins.}
journal = []
volume = {293:12}
journal type = {AC}
place = {France}
year = {1981}
month = {Nov}
}
title = {Uranium-phosphate relationship in phosphated chalks of the Mons and Picardie Bassins}
author = {Quinif, Y, Charlet, J M, Dupuis, C, and Robaszynski, F}
abstractNote = {The lithological and geochemical conditions relative to the ''Senonian'' phosphatic chalks are relatively simple in the Basins of Mons (Belgium) and of Picardy (France). Their characteristics permit us to study chiefly the uranium-phosphate relation. It appears a very good linear correlation between the phosphate and the uranium. The coefficient U/P/sub 2/O/sub 5/ remains a constant from the bottom to the top of the same section, but changes in space for synchronic formations (lateral variation of geochemical facies) and in time for two separated basins.}
journal = []
volume = {293:12}
journal type = {AC}
place = {France}
year = {1981}
month = {Nov}
}