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Quantifying lithological variability in the mantle

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TLDR
In this article, the authors present a method that can be used to estimate the amount of recycled material present in the source region of mid-ocean ridge basalts by combining three key constraints: (1) the melting behaviour of the lithologies identified to be present in a mantle source, (2) the overall volume of melt production, and (3) the proportion of the melt production attributable to melting of each lithology.
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This article is published in Earth and Planetary Science Letters.The article was published on 2014-06-01 and is currently open access. It has received 109 citations till now. The article focuses on the topics: Iceland plume & Mantle wedge.

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Global variations in abyssal peridotite compositions

TL;DR: In this paper, a compilation of abyssal peridotite geochemical data (modes, mineral major elements, and clinopyroxene trace elements) for > 1200 samples from 53 localities on 6 major ridge systems is presented.
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The role of pyroxenite in basalt genesis: Melt-PX, a melting parameterization for mantle pyroxenites between 0.9 and 5 GPa

TL;DR: In this paper, a new parameterization, Melt-PX, was developed to predict near-solidus temperatures and extents of melting as a function of temperature and pressure for mantle pyroxenites.

Plume-driven Upwelling Under Central Iceland

TL;DR: A suite of 70 basaltic samples from the Herdubreid region of the Northern Volcanic Zone (NVZ) in central Iceland has been analysed for major and trace element compositions as mentioned in this paper.
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Global distribution of sediment-hosted metals controlled by craton edge stability

TL;DR: This paper found that 85% of sediment-hosted base metals, including all giant deposits (>10 megatonnes of metal, occur within 200 kilometres of the transition between thick and thin lithosphere.
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Sulfur solubility in reduced mafic silicate melts: Implications for the speciation and distribution of sulfur on Mercury

TL;DR: In this article, an empirical parameterization was developed to predict sulfide saturation (SCSS) in Mercurian magmas as a function of oxygen fugacity ( f O 2 ), temperature, pressure and silicate melt composition.
References
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Book

Numerical Recipes in FORTRAN

TL;DR: The Diskette v 2.04, 3.5'' (720k) for IBM PC, PS/2 and compatibles [DOS] Reference Record created on 2004-09-07, modified on 2016-08-08.
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An internally consistent thermodynamic data set for phases of petrological interest

TL;DR: In this paper, the thermodynamic properties of 154 mineral endmembers, 13 silicate liquid end-members and 22 aqueous fluid species are presented in a revised and updated data set.
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Mantle geochemistry: the message from oceanic volcanism

TL;DR: Basaltic volcanism'samples' the Earth's mantle to great depths, because solid-state convection transports deep material into the (shallow) melting region as mentioned in this paper.
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Convection Plumes in the Lower Mantle

TL;DR: The concept of crustal plate motion over mantle hotspots has been advanced to explain the origin of the Hawaiian and other island chains and the origin the Walvis, Iceland-Farroe and other aseismic ridges as discussed by the authors.
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