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Figures8and9show the effects of the porosity parameter on the radial and tangential components of the velocity profile. The enhancement in the porous parameter of the fluid is because of an increment of the fluid viscosity or reduction in the permeability at the edge, this will result in a gr...
Iron and REE contents are lower in the centre. Consistently, REE patterns also change systematically from the rim to the centre. These can plausibly be interpreted as the result of hydrothermal metasomatism of a calcite/dolomite grain by Fe-, Mg- and REE-enriched fluids. ...
Thematic Section: Green Rare Earth Elements--Innovations in Ore Processing, Hydrometallurgy, and Electrolysis Open access Published: 20 September 2016 Volume 3, pages 122–149, (2017) Cite this article Download PDF You have full access to this open access article ...
Diverse magma evolution recorded in trace element composition of zircon from Permo-Carboniferous rhyolites (NE German Basin, NW Polish Basin) ArticleOpen access15 September 2023 High-spatial resolution dating of monazite and zircon reveals the timing of subduction–exhumation of the Vaimok Lens in the...
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Furthermore, assigning a diagenetic environment of formation (deep-burial versus shallow-burial) based exclusively on textural descriptions can also result in misleading interpretations. Hydrothermal dolomitizing fluids, usually generated at depth, may ascend through fractures or faults, and evolve through ...
The decomposition and adsorption of organic matter and oxidation conditions are considered the main factors for the fractionation of REE in pore water [15]. REE enrichment in the deep-sea sediments is explained as the result of the interaction of several factors: low sedimentation rate, the presen...
REE enrichment in the deep-sea sediments is explained as the result of the interaction of several factors: low sedimentation rate, the presence of phosphate component near the seawater/sediment interface, high REE of the bottom seawater, oxidation conditions, certain bottom current conditions, and ...