LOW-TEMPERATURE AQUEOUS MOBILITY OF THE RARE-EARTH ELEMENTS DURING SANDSTONE DIAGENESIS

被引:29
|
作者
BOUCH, JE [1 ]
HOLE, MJ [1 ]
TREWIN, NH [1 ]
MORTON, AC [1 ]
机构
[1] BRITISH GEOL SURVEY,KEYWORTH NG12 5GG,NOTTS,ENGLAND
关键词
NORTH SEA; DIAGENESIS; FRANCOLITE; RARE EARTHS; ND-144/ND-143;
D O I
10.1144/GSL.JGS.1995.152.01.01
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Diagenetic francolite (carbonate fluor-apatite) occurs as over-growths on detrital apatite grains in sandstones from the Loner Jurassic Statfjord Formation of the North Sea. The francolite overgrowths are considerably more enriched in the rare-earth elements (up to I wt % Ce2O3), Sr and F than the detrital cores. These elements were carried in aqueous solution, probably in the form of complex Ligands involving organically sourced carbon and halogens. It is possible that reported aberrant neodymium isotope model ages within the Statfjord Formation are the result of mobilization and relative fractionation of Sm and Nd during diagenesis, rather than a result of changes in provenance.
引用
收藏
页码:895 / 898
页数:4
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