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Journal ArticleDOI

Isotopic and trace element composition of volcanic glasses from the Akaki Canyon, Cyprus: implications for the origin of the Troodos ophiolite

TLDR
In this article, the Akaki River section of the Troodos ophiolite complex was analyzed and the major elements, K, Rb, Cs, Sr, Ba, Sc, Cr, Ni, Hf, Ta, Th, and REE concentrations and isotopic compositions of carefully hand-picked volcanic glasses were reported.
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This article is published in Earth and Planetary Science Letters.The article was published on 1985-11-01. It has received 190 citations till now. The article focuses on the topics: Troodos Ophiolite & Incompatible element.

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Ophiolite genesis and global tectonics: Geochemical and tectonic fingerprinting of ancient oceanic lithosphere

TL;DR: A review of these ideas as well as a new classification of ophiolites, incorporating the diversity in their structural architecture and geochemical signatures that results from variations in petrological, geochemical, and tectonic processes during formation in different geodynamic settings is presented in this article.
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ICP-MS — A powerful tool for high-precision trace-element analysis in Earth sciences: Evidence from analysis of selected U.S.G.S. reference samples

TL;DR: In this article, the power of inductively coupled plasma-mass spectrometry (ICP-MS) is demonstrated for petrogenetic studies using a simple HF-HNO3 dissolution in screwtop Teflon® bombs.
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Immobile Element Fingerprinting of Ophiolites

TL;DR: In this paper, immobile element proxies for fractionation indices, alkalinity, mantle temperature, mantle flow and subduction addition are used to classify ophiolite lavas and fingerprint the precise setting of the ridge at which an ophiola formed.
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Birth, death, and resurrection: The life cycle of suprasubduction zone ophiolites

TL;DR: A consistent sequence of events during their formation and evolution that suggests that they form in response to processes that are common to all such ophiolites has been found in this article.
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Temperatures and H 2 O contents of low-MgO high-alumina basalts

TL;DR: Experimental evidence was used to estimate H2O contents in low-MgO high-alumina basalts (HABs) (8.5wt.% MgO) as discussed by the authors.
References
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Journal ArticleDOI

The use of bromine pentafluoride in the extraction of oxygen from oxides and silicates for isotopic analysis

TL;DR: In this paper, a technique was developed in which bromine pentafluoride was used as a reagent for quantitative liberation of oxygen from oxides and silicates, and the results of isotopic analyses were compared with measurements made in other laboratories by other procedures.
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Determination of REE, Ba, Fe, Mg, Na and K in carbonaceous and ordinary chondrites

TL;DR: In this paper, the exact determination of REE and Ba abundances in three carbonaceous (Orgueil Cl, Murchison C2 and Allende C3) and seven olivine-bronzite chondrites were carried out by mass spectrometric isotope dilution technique.
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Variation of seawater 87Sr/86Sr throughout Phanerozoic time

TL;DR: In this paper, a curve of seawater 87Sr/86Sr versus geologic time through the Phanerozoic is presented, which provides a basis for dating many marine carbonate, evaporite, and phosphate samples.
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Lead isotopic study of young volcanic rocks from mid-ocean ridges, ocean islands and island arcs

TL;DR: Lead isotopic compositions of young volcanic rocks from different tectonic environments have distinctive characteristics their differences are evaluated within the framework of global tectonics and mantle differentiation Ocean island leads are in general more radiogenic than mid-ocean ridge basalt (morb) leads as discussed by the authors.
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Solar-system abundances of the elements

TL;DR: In this paper, the Ogueil Cl meteorite and all previous Cl chondrite analyses were employed to develop a new solar system abundance table, including the standard deviation and number of analyses for each element.
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