A weathering profile on a uniform Lower Cretaceous volcanogenic sandstone from southern Victoria, Australia is enriched in rare-earth elements (REE), Y and other elements including Ba, Sr and Rb. Enrichments of REE of up to 7 times parent-rock values are associated with Fe-leached members of alteration couplets with little or no enrichment in adjacent Fe-rich members. These alteration couplets are similar in appearance to Liesegang banding. The REE have been fractionated during accumulation, leading to relative enrichment of the light rare earths (LREE).
The formation of an alteration couplet from fresh rock at the weathering front involves redistribution of only Fe (and P) and does not involve redistribution of REE, Y. Ba, Sr and Rb. Breakdown of original minerals in the present soil and degradation of vermiculite in the upper part of the weathering profile releases RE and related elements into solution. This solution moves down and along the profile until it comes into contact with neutral to alkaline conditions at the narrow weathering front. Here REE particularly are absorbed and apparently fixed in vermiculite forming at the expense of biotite and chlorite. (La + Ce + Nd + Y) up to 10.1 wt.% is recorded in degraded biotite grains with similar but lower contents in the degraded diagenetic chlorite cement.
Such accumulation and fractionation have important implications for REE studies involving sedimentary rocks or for that matter outcrop samples of any rock type. 相似文献
