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Cited by 229

The DOI matches its Crossref record; 3 of the 3 references it cites were found in a registry or an index.

Diapiric Flow at Subduction Zones: A Recipe for Rapid Transport

Open access
Hall, Paul S., Kincaid, Chris·2001·Science

Abstract

Recent geochemical studies of uranium-thorium series disequilibrium in rocks from subduction zones require magmas to be transported through the mantle from just above the subducting slab to the surface in as little as ∼30,000 years. We present a series of laboratory experiments that investigate the characteristic time scales and flow patterns of the diapiric upwelling model of subduction zone magmatism. Results indicate that the interaction between buoyantly upwelling diapirs and subduction-induced flow in the mantle creates a network of low-density, low-viscosity conduits through which buoyant flow is rapid, yielding transport times commensurate with those indicated by uranium-thorium studies.

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Crossref · 10.1126/science.1060488

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Metadata

Authors
Hall, P. S., & Kincaid, C.
Venue
Science
Published
2001-06-29
Volume
292
Issue
5526
Pages
2472-2475
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1995464473
Cited by
229
References
3
FWCI
9.78
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Diapiric Flow at Subduction Zones: A Recipe for Rapid Transport. https://app.cochat.ai/papers/10.1126/science.1060488
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Hall, P. S., & Kincaid, C. (2001). Diapiric Flow at Subduction Zones: A Recipe for Rapid Transport. Science. https://doi.org/10.1126/science.1060488

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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.