Journal ArticleDOI
Solution properties of rare earth elements in silicate melts: Inferences from immiscible liquids
Adam James Ellison,Paul C. Hess +1 more
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In this paper, the authors investigated the partitioning behavior of rare earth elements (REE) between immiscible silicate liquids and found that REE preferentially partition into the end-member liquids that are rich in network-modifying cations.About:
This article is published in Geochimica et Cosmochimica Acta.The article was published on 1989-08-01. It has received 48 citations till now. The article focuses on the topics: Silicate minerals & Partition coefficient.read more
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Compositions of the Apatite-Group Minerals: Substitution Mechanisms and Controlling Factors
Yuanming Pan,Michael E. Fleet +1 more
TL;DR: More than 100 compounds with the apatite structure have been synthesized as mentioned in this paper, and more than 1000 compounds have been designed to synthesize apatites in the last few decades.
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Experimental studies of trace-element partitioning applicable to igneous petrogenesis — Sedona 16 years later
TL;DR: In the 16 years since the Sedona Conference on the behavior of trace elements in silicate systems, numerous studies providing new data have filled many of the gaps in knowledge of trace-element partitioning evident at that conference.
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A model for monazite/ melt equilibrium and application to the generation of granitic magmas
TL;DR: In this article, the authors proposed an equation for the equilibrium between monazite and Ca-poor felsic melts, which can be used as a thermometer, based on the total rare-earth elements (REE) content of natural magmatic rocks.
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Trace element partitioning between apatite and silicate melts
Stefan Prowatke,Stephan Klemme +1 more
TL;DR: In this paper, the apatite/melt trace element partition coefficients for a large number of trace elements (Cs, Rb, Ba, La, Ce, Pr, Sm, Gd, Lu, Y, Sr, Zr, Hf, Nb, Ta, U, Pb, and Th) were presented.
A model for monazite/melt equilibrium and application to the generation of granitic magmas
TL;DR: In this article, the authors proposed an equation for the equilibrium between monazite and Ca-poor felsic melts, which can be used as a thermometer, based on the total rare-earth elements (REE) content of natural magmatic rocks.
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Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides
TL;DR: The effective ionic radii of Shannon & Prewitt [Acta Cryst. (1969), B25, 925-945] are revised to include more unusual oxidation states and coordinations as mentioned in this paper.
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The viscosity of magmatic silicate liquids; a model calculation
Y. Bottinga,D. F. Weill +1 more
TL;DR: In this article, a linear equation of the form ln h = Si Xi Di, where h is the Newtonian viscosity coefficient, Xi is the mole fraction of oxide component i, and Di is an empirical constant associated component i over a restricted range of SiO 2 concentration, was used to calculate the viscosities of many natural magmatic liquids.
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Large partition coefficients for trace elements in high-silica rhyolites
Gail A. Mahood,Wes Hildreth +1 more
TL;DR: In this paper, the partitioning of 25 trace elements between high-silica rhyolitic glass and unzoned phenocrysts of potassic and sodic sanidine, biotite, augite, ferrohedenbergite, hypersthene, fayalite, titanomagnetite, ilmenite, zircon, and allanite has been determined by INAA on suites of samples from the mildly peralkaline lavas and tuff of the Sierra La Primavera, Mexico, and the metaluminous, compo