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Journal ArticleDOI

Two-dimensional thermo-kinetic model for the olivine-spinel phase transition in subducting slabs

TLDR
In this paper, the effects of the latent heat release on the kinetics of the olivine-spinel phase transition were investigated and the role of the thermo-kinetic coupling process was clarified.
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This article is published in Physics of the Earth and Planetary Interiors.The article was published on 1996-04-01. It has received 46 citations till now. The article focuses on the topics: Phase transition & Phase boundary.

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Citations
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Influence of trench width on subduction hinge retreat rates in 3‐D models of slab rollback

TL;DR: In this article, the authors investigate the time evolution of a progressive rollback subduction, measure the accompanying return flow in the upper mantle, and quantify the plate kinematics, showing that most of the negative buoyancy of the subducting slab is converted into a toroidal flow, and the remaining amount goes into driving flow parallel to displacement of the slab.
Journal ArticleDOI

Rheological structure and deformation of subducted slabs in the mantle transition zone: implications for mantle circulation and deep earthquakes

TL;DR: In this paper, the authors investigated the rheological structure of subducted slabs of oceanic lithosphere in the mantle transition zone based on mineral physics observations incorporating grain-size, stress, temperature and pressure dependence of rheology.
Journal ArticleDOI

On the role of subducting oceanic plateaus in the development of shallow flat subduction.

TL;DR: In this paper, a numerical thermochemical convection model was used to simulate the subduction of an oceanic lithosphere that contains an 18 km-thick oceanic crustal plateau of 18-km thickness.
Journal ArticleDOI

Grain-size evolution in subducted oceanic lithosphere associated with the olivine-spinel transformation and its effects on rheology

TL;DR: In this paper, the role of grain-size reduction during the olivine-spinel transformation on rheological properties of subducting slabs on the basis of a scaling model for microstructural development during nucleation and growth was investigated.
Journal ArticleDOI

Experimental constraints on the depth of olivine metastability in subducting lithosphere

TL;DR: In this article, the authors derived new thermo-kinetic subduction zone models to predict the extent of olivine metastability within the stability fields of its high-pressure polymorphs, wadsleyite and ringwoodite.
References
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Journal ArticleDOI

Kinetics of Phase Change. I General Theory

TL;DR: In this paper, the theory of phase change is developed with the experimentally supported assumptions that the new phase is nucleated by germ nuclei which already exist in the old phase, and whose number can be altered by previous treatment.
Journal ArticleDOI

Kinetics of Phase Change. II Transformation‐Time Relations for Random Distribution of Nuclei

TL;DR: In this article, a relation between the actual transformed volume V and a related extended volume V1 ex is derived upon statistical considerations, and a rough approximation to this relation is shown to lead, under the proper conditions, to the empirical formula of Austin and Rickett.
Journal ArticleDOI

Granulation, Phase Change, and Microstructure Kinetics of Phase Change. III

TL;DR: In this paper, a comprehensive description of the phenomena of phase change may be summarized in Phase Change, Grain Number and Microstructure Formulas or Diagrams, giving, respectively, the transformed volume, grain, and microstructure densities as a function of time, temperature, and other variables.
Book

The theory of transformations in metals and alloys

J.W. Christian, +1 more
TL;DR: In this paper, the authors present a general introduction to the theory of transformation kinetics of real metals, including the formation and evolution of martensitic transformations, as well as a theory of dislocations.
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