Search results for "Eu anomaly"

showing 2 items of 2 documents

Mineralogical and chemical variability of fluvial sediments: 1. Bedload sand (Ganga–Brahmaputra, Bangladesh)

2010

This study investigates the natural processes that control concentration of detrital minerals and consequently chemical elements in river sand. The novelty of our approach consists in the systematic integration of detailed textural, petrographical, mineralogical and chemical data, and in the quantitative description and modeling of relationships among mineralogical and chemical variables for each sample and each grain-size class in each sample. Bed sediment in transit in the largest sedimentary system on Earth chiefly consists of fine-grained lithofeldspatho quartzose sand including rich amphibole–epidote–garnet suites, mixed with minor very-fine grained-sand to silt subpopulations containi…

Sedimentary petrologyProvenanceHimalayaGeochemistrysedimentary geochemistry sedimentary petrology settling equivalence selective entrainment placer sands opaque minerals REE-bearing minerals Eu anomaly HimalayaSedimentFluvialEu anomalyWeatheringSiltSedimentary geochemistryGeophysicsPlacer sandSettling equivalenceSpace and Planetary ScienceGeochemistry and PetrologyOpaque mineralEarth and Planetary Sciences (miscellaneous)Sedimentary rockGEO/02 - GEOLOGIA STRATIGRAFICA E SEDIMENTOLOGICAREE-bearing mineralSelective entrainmentChemical compositionGeologyBed load
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Geochemistry of Zr, Hf, and REE in a wide spectrum of Eh and water composition: The case of Dead Sea Fault system (Israel)

2017

International audience; Along the Jordan Valley-Dead Sea Fault area several natural waters in springs, wells, and catchments occur. The chemical-physical characters of the studied waters allowed for the first time the investigation of the Zr and Hf geochemical behavior, apart from REE, extended to a wide range of Eh, temperature, salinity, and pH conditions. The results of this study indicate that the dissolved Zr and Hf distribution in natural waters is strongly influenced by redox conditions since these in turn drive the deposition of Fe-oxyhydroxides or pyrite. In oxidizing waters saturated or oversaturated in Fe-oxyhydroxides (Group 1), superchondritic Zr/Hf values are measured. On the …

Geochemistry and PetrologyZr/Hf fractionationCe anomaly[SDU]Sciences of the Universe [physics]Eu anomalyREE distributionGeophysic
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