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Cited by 538

The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.

On the Thermal Balance of a Mid-Ocean Ridge

Open access
Lister, C. R. B.·1972·Geophysical Journal International

Abstract

The northernmost expressions of the East Pacific Rise spreading centre, the Juan de Fuca Ridge and Explorer Trough, have unusual heat-flow distributions. Crestal values are only moderately high, but flank areas that are models of undisturbed sedimentation have mean heat flows near 7 HFU (290 mW m−2). The values in these areas retain considerable scatter, but the detailed distribution is close to the opposite of that expected from conductive heat-flow refraction. The high mean values confirm that sea-floor spreading occurs by the upwelling of hot (magma temperature) material. The low crestal measurements and the non-refractive scatter in the flank areas strongly suggest that hydrothermal circulation is the dominant heat transfer process in fresh crestal material. Much of the heat loss from the new lithospheric material must occur through open circulation near the ridge crest and is never reflected in measurements of surface conduction.

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Crossref · 10.1111/j.1365-246x.1972.tb05766.x

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Metadata

Authors
Lister, C. R. B.
Venue
Geophysical Journal International
Published
1972-04
Volume
26
Issue
5
Pages
515-535
ISSN
  • 0956-540X (ISSN-L)
  • 1365-246X
OpenAlex
W2039443168
Cited by
538
References
2
FWCI
24.54
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: On the Thermal Balance of a Mid-Ocean Ridge. https://app.cochat.ai/papers/10.1111/j.1365-246x.1972.tb05766.x
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Lister, C. R. B. (1972). On the Thermal Balance of a Mid-Ocean Ridge. Geophysical Journal International. https://doi.org/10.1111/j.1365-246x.1972.tb05766.x

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