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Cited by 315

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Mantle Convection with Plates and Mobile, Faulted Plate Margins

Zhong, Shijie, Gurnis, Michael·1995·Science

Abstract

A finite-element formulation of faults has been incorporated into time-dependent models of mantle convection with realistic rheology, continents, and phase changes. Realistic tectonic plates naturally form with self-consistent coupling between plate and mantle dynamics. After the initiation of subduction, trenches rapidly roll back with subducted slabs temporarily laid out along the base of the transition zone. After the slabs have penetrated into the lower mantle, the velocity of trench migration decreases markedly. The inhibition of slab penetration into the lower mantle by the 670-kilometer phase change is greatly reduced in these models as compared to models without tectonic plates.

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Crossref · 10.1126/science.267.5199.838

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Metadata

Authors
Zhong, S., & Gurnis, M.
Venue
Science
Published
1995-02-10
Volume
267
Issue
5199
Pages
838-843
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1997541643
Cited by
315
References
1
FWCI
15.54
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Mantle Convection with Plates and Mobile, Faulted Plate Margins. https://app.cochat.ai/papers/10.1126/science.267.5199.838
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Zhong, S., & Gurnis, M. (1995). Mantle Convection with Plates and Mobile, Faulted Plate Margins. Science. https://doi.org/10.1126/science.267.5199.838

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.