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Applications of PGE Radioisotope Systems in Geo
Applications of PGE Radioisotope Systems in Geo

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The cold and relatively dry nature of mantle forearcs in subduction
The cold and relatively dry nature of mantle forearcs in subduction

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Evidence for mantle metasomatism by hydrous silicic - HAL-Insu
Evidence for mantle metasomatism by hydrous silicic - HAL-Insu

... far produced in H2O-added melting experiments on basalts up to 30 kbar 11-13 display a broad negative trend that completely overlaps that field of natural glasses or veins believed to be slab melts 6,7, in contrast to results from dehydration melting experiments 13-15 (Fig. 2b). A similar feature is ...
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Homework Assignment #2: Plate Tectonics and

... i. What major layer is the asthenosphere part of? Important Clarification of What the Book Says: The asthenosphere acts like a layer of grease between the cold rigid lithosphere above and the relatively stiff mantle layers below, allowing the “plates” (large slabs of lithosphere) to move independent ...
“Excess Argon”: The “Archilles` Heel” of Potassium
“Excess Argon”: The “Archilles` Heel” of Potassium

... dating of rocks has been crucial in underpinning the billions of years for Earth history claimed by evolutionists. Critical to these dating methods is the assumption that there was no radiogenic argon (40Ar*) in the rocks (e.g., basalt) when they formed, which is usually stated as self-evident. Dalr ...
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Mantle plume



A mantle plume is a mechanism proposed in 1971 to explain volcanic regions of the earth that were not thought to be explicable by the then-new theory of plate tectonics. Some such volcanic regions lie far from tectonic plate boundaries, for example, Hawaii. Others represent unusually large-volume volcanism, whether on plate boundaries, e.g. Iceland, or basalt floods such as the Deccan or Siberian traps.A mantle plume is posited to exist where hot rock nucleates at the core-mantle boundary and rises through the Earth's mantle becoming a diapir in the Earth's crust. The currently active volcanic centers are known as ""hot spots"". In particular, the concept that mantle plumes are fixed relative to one another, and anchored at the core-mantle boundary, was thought to provide a natural explanation for the time-progressive chains of older volcanoes seen extending out from some such hot spots, such as the Hawaiian–Emperor seamount chain.The hypothesis of mantle plumes from depth is not universally accepted as explaining all such volcanism. It has required progressive hypothesis-elaboration leading to variant propositions such as mini-plumes and pulsing plumes. Another hypothesis for unusual volcanic regions is the ""Plate model"". This proposes shallower, passive leakage of magma from the mantle onto the Earth's surface where extension of the lithosphere permits it, attributing most volcanism to plate tectonic processes, with volcanoes far from plate boundaries resulting from intraplate extension.
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