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Chrome spinel-hosted melt inclusions in Paleoproterozoic primitive volcanic rocks, northern Finland: Evidence for coexistence and mixing of komatiitic and picritic magmas

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TLDR
In this article, the authors investigated the compositional features of the ultramafic volcanic rocks at the time of melt entrapment and found a good correlation between the major element compositions of the melt inclusions and their host spinels, with picritic melts being found in high-Ti spinels and komatiitic melts in low-Ti spinsels.
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This article is published in Chemical Geology.The article was published on 2013-04-08. It has received 18 citations till now. The article focuses on the topics: Melt inclusions & Incompatible element.

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Deep hydrous mantle reservoir provides evidence for crustal recycling before 3.3 billion years ago

TL;DR: Hydrogen isotopes and compositions of melt inclusions in olivine in komatiites indicate a hydrous source produced by recycling of seawater-altered crust into the deep mantle over 3.3 billion years ago, which implies that a deep hydrous mantle reservoir has been present in the Earth's interior since at least the Palaeoarchaean era.
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Archaean andesite petrogenesis: Insights from the Grædefjord Supracrustal Belt, southern West Greenland

TL;DR: In this paper, the authors presented new whole-rock major, trace and platinum-group element data for meta-volcanic rocks from the Mesoarchaean Graedefjord Supracrustal Belt (GSB), located within the Tasiusarsuaq terrane, southern West Greenland.
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Polymineralic inclusions in mantle chromitites from the Oman ophiolite indicate a highly magnesian parental melt

TL;DR: In this article, polymineralic inclusions interpreted as melt inclusions in chromite from the dunitic Moho Transition Zone in the Maqsad area of the Oman ophiolite have been analysed and compositions integrated using a rastering technique on the scanning electron microscope.
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Empirical constraints on partitioning of platinum group elements between Cr-spinel and primitive terrestrial magmas

TL;DR: In this article, the authors investigated the role of Cr-spinel fractional crystallization on the PGE geochemistry of primitive crspinel, measured by LA-ICP-MS, from nine volcanic suites covering various tectonic settings including island arc picrites, boninites, large igneous province picrites and mid-ocean ridge basalts.
References
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Chemical and isotopic systematics of oceanic basalt : implications for mantle composition and processes

S. S. Sun
TL;DR: In this article, trace-element data for mid-ocean ridge basalts and ocean island basalts are used to formulate chemical systematics for oceanic basalts, interpreted in terms of partial-melting conditions, variations in residual mineralogy, involvement of subducted sediment, recycling of oceanic lithosphere and processes within the low velocity zone.
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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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Neodymium isotopes in the Colorado Front Range and crust–mantle evolution in the Proterozoic

TL;DR: In this article, an empirical model is constructed that may provide accurate crust-formation ages f or rocks of all ages, based on the isotopic data of major rock types of the basement underlying the Rocky Mountains in Colorado.
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Inter-laboratory note. Laser ablation inductively coupled plasma mass spectrometric transient signal data acquisition and analyte concentration calculation

TL;DR: In this paper, the authors discuss data acquisition and reduction considerations in LA-ICP-MS analysis and suggest optimum data acquisition parameters for time-resolved data acquisition, sensitivity calibration is obtained from reference materials with known analyte concentrations and naturally occurring internal standards are used to correct for the multiplicative correction factors.
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