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Cited by 309

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

Mantle Plumes and Continental Tectonics

Hill, R. I., Campbell, I. H., Davies, G. F., Griffiths, R. W.·1992·Science

Abstract

Mantle plumes and plate tectonics, the result of two distinct modes of convection within the Earth, operate largely independently. Although plumes are secondary in terms of heat transport, they have probably played an important role in continental geology. A new plume starts with a large spherical head that can cause uplift and flood basalt volcanism, and may be responsible for regional-scale metamorphism or crustal melting and varying amounts of crustal extension. Plume heads are followed by narrow tails that give rise to the familiar hot-spot tracks. The cumulative effect of processes associated with tail volcanism may also significantly affect continental crust.

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Crossref · 10.1126/science.256.5054.186

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Metadata

Authors
Hill, R. I., Campbell, I. H., Davies, G. F., & Griffiths, R. W.
Venue
Science
Published
1992-04-10
Volume
256
Issue
5054
Pages
186-193
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1981819665
Cited by
309
References
3
FWCI
16.58
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Mantle Plumes and Continental Tectonics. https://app.cochat.ai/papers/10.1126/science.256.5054.186
The paper
Hill, R. I., Campbell, I. H., Davies, G. F., & Griffiths, R. W. (1992). Mantle Plumes and Continental Tectonics. Science. https://doi.org/10.1126/science.256.5054.186

Data sources

Bibliographic data: Semantic Scholar, OpenAlex, Crossref.

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.