Abstract
We analyzed the mineralogical and chemical (including rare earth element [REE]) composition of the >63, 32-63, and 63 œm fraction is enriched in SiO2 when compared to average Upper Continental Crust (UCC). The trace element contents of the 63 œm fraction shows lower contents. The chondrite-normalized REE distribution patterns are remarkably similar for all grain size fractions, with a general enrichment of the LREEs and a negative Eu anomaly. The >63 œm fractions have the lowest REE abundances, no LREE-HREE fractionation, but show a small negative Eu anomaly. The 63 œm fraction. The Eu/Eu*, Th/Sc, and Rb/Sr ratios of the
| Original language | English |
|---|---|
| Pages (from-to) | 73-86 |
| Number of pages | 14 |
| Journal | Chemie der Erde / Geochemistry |
| Volume | 62 |
| Issue number | 1 |
| Publication status | Published - 2002 |
Austrian Fields of Science 2012
- 1051 Geology, Mineralogy
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