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Journal ArticleDOI

Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphere

TLDR
In this paper, the influence of water on the dynamics of the oceanic upper mantle is re-evaluated based on recent experimental constraints on the solubility of water in mantle minerals and earlier experimental studies of olivine rheology.
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This article is published in Earth and Planetary Science Letters.The article was published on 1996-10-01. It has received 1414 citations till now. The article focuses on the topics: Mantle wedge & Mantle (geology).

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Citations
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Journal ArticleDOI

Major and trace element composition of the depleted MORB mantle (DMM)

TL;DR: Asimow et al. as mentioned in this paper derived an estimate for the chemical composition of the depleted MORB mantle (DMM), the source reservoir to mid-ocean ridge basalts (MORBs), which represents at least 30% the mass of the whole silicate Earth.
Book ChapterDOI

Rheology of the Upper Mantle and the Mantle Wedge: A View from the Experimentalists

TL;DR: In this paper, the authors provide a critical review of flow law parameters for olivine aggregates and single crystals deformed in the diffusion creep and dislocation creep regimes under both wet and dry conditions.
Journal ArticleDOI

The mean composition of ocean ridge basalts

TL;DR: In this article, the mean composition of mid-ocean ridge basalts (MORB) is determined using a global data set of major elements, trace elements, and isotopes compiled from new and previously published data.
Journal ArticleDOI

The global range of subduction zone thermal models

TL;DR: In this article, a suite of thermal models for the global subduction system is presented, where the authors model 56 segments of subduction zones using kinematically defined slabs based on updated geometries from Syracuse and Abers (2006).
Journal ArticleDOI

An olivine-free mantle source of Hawaiian shield basalts

TL;DR: Modelling shows that more than half of Hawaiian magmas formed during the past 1 Myr came from a deep olivine-bearing source, and the proportion of recycled (oceanic) crust varies from 30 per cent near the plume centre to insignificant levels at the plumes edge.
References
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Journal ArticleDOI

An analysis of the variation of ocean floor bathymetry and heat flow with age

TL;DR: In this paper, a simple cooling model and the plate model were proposed to account for the variation in depth and heat flow with increasing age of the ocean floor. But the results were limited to the North Pacific and North Atlantic basins.
Journal ArticleDOI

Trace element fractionation during anatexis

TL;DR: The theoretical basis of trace element fractionation presented in a paper by P. W. Gast (1968) can be developed in a more flexible algebraic form, which is described and illustrated in this article.
Journal ArticleDOI

Rheology of the Upper Mantle: A Synthesis

TL;DR: A synthesis of laboratory studies and geophysical and geological observations shows that transitions between diffusion and dislocation creep likely occur in the Earth's upper mantle.
Journal ArticleDOI

Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness

TL;DR: In this paper, the global major element variations can be explained by ∼8-20% melting of the mantle at associated mean pressures of 5-16 kbar, and the lowest extents of melting occur at shallowest depths in the mantle and are associated with the deepest ocean ridges.
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