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Richard Hinton

Researcher at University of Edinburgh

Publications -  37
Citations -  2800

Richard Hinton is an academic researcher from University of Edinburgh. The author has contributed to research in topics: Zircon & Silicic. The author has an hindex of 25, co-authored 37 publications receiving 2451 citations.

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Carbonatite Metasomatism of the Oceanic Upper Mantle: Evidence from Clinopyroxenes and Glasses in Ultramafic Xenoliths of Grande Comore, Indian Ocean

TL;DR: Petrological and geochemical data for a suite of brought down in a subducting slab at a former convergent plate ultramafic xenoliths (lherzolites and wehrlites) from La Grille margin is presented in this article.
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The chemistry of zircon: Variations within and between large crystals from syenite and alkali basalt xenoliths

TL;DR: In this article, Trace element analyses have been made of large zircon crystals from rocks of alkaline affinities by ion microprobe and the partition coefficients for the light rare earth elements (LREEs), between zircons and melt or whole rock, must therefore be significantly lower than those calculated using bulk analyses.
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Annual to sub-annual resolution of multiple trace-element trends in speleothems

TL;DR: In this paper, an ion microprobe analysis of speleothems reveals that annual to sub-annual variations in element chemistry exist at five, shallow western European cave sites (Crag Cave, County Kerry and Ballynamintra, County Waterford, Ireland; Uamh an Tartair, Sutherland, Scotland; Grotte Pere-Noel, Belgium; Grotta di Ernesto, NE Italy) with widely varying climatic, geomorphic and geological settings.
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Apatite: A new redox proxy for silicic magmas?

TL;DR: In this article, the authors explored the use of Mn in apatite as an oxybarometer in intermediate and silicic igneous rocks and found that increased Mn concentrations in apats correlate with decreasing Fe2O3 (Fe3+) and Mn in the whole-rock and likely reflect increased Mn2+/Mn3+ and greater compatibility of Mn2+, relative to Mn3+ in apatis under reduced conditions.