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Magmatic processes: Physicochemical principles: Edited by B. O. Mysen. The Geochemical Society, spec. pub. no. 1, 1987, 500p., $45.00 (Geochemical Society Members), $65.00 (other). (ISBN 0-941809-005)

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This article is published in Geochimica et Cosmochimica Acta.The article was published on 1988-04-01. It has received 238 citations till now.

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Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere

TL;DR: In this paper, a pyrolitic GPa from a mantle enriched in SiO2 relative to pyrolite was made from 3 to 7 GPa in piston-cylinder and multi-anvil apparatus.
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Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth

TL;DR: Measurements of the composition of fluids and melts equilibrated with a basaltic eclogite at pressures equivalent to depths in the Earth and temperatures of 700–1,200 °C constrain the recycling rates of key elements in subduction-zone arc volcanism.
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An experimental determination of primary carbonatite magma composition

TL;DR: In this paper, the phase relationship of carbonate and amphibole-bearing peridotite (containing 0.3% H2O and 0.5-2.5% CO2) is investigated.
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Mantle metasomatism by ephemeral carbonatite melts

TL;DR: In this paper, the authors show that carbonatite melts will alter the chemical composition of the mantle through which they pass, producing distinctive mineralogical and geochemical signatures, which can be recognized in peridotite xenolith suites from Australia.
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Energy-constrained open-system magmatic processes I : General model and energy-constrained assimilation and fractional crystallization (EC-AFC) formulation

TL;DR: In this article, a general class of models (EC-AFC) is presented, where energy-constrained models have the of geochemical paths for trace elements and isotopic ratios for magma taking advantage of linking thermal and chemical properties of magma undergoing simultaneous replenishment, assimilation and fractional chambers.
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