Introduction

Background and implications of the linear heat flow‐heat production relationship

Paul Morgan, Wayne N. Sawka, Kevin Patrick Furlong

Research output: Contribution to journalArticle

21 Citations (Scopus)

Abstract

The discovery in the late 1960s of the linear heat flow‐heat production relationship was a major advance in the understanding of the thermal structure of continents. However, although heat flow provinces have now been defined in all continents except Antarctica, the full implications of the relationship to deep thermal structure and the limitations of the relationship to applications in all terranes are not yet clear. In addition, despite major advances in the geochemical factors controlling the distribution of heat production in the crust, a geochemical rationale for the relationship is lacking. The relationship was originally interpreted in terms of one‐dimensional models, but new two‐ and three‐dimensional model studies suggest more complex interpretations in terms of lower crustal heat flow. Contributions to these problems in this special issue represent new observational, geochemical and modeling studies of the relationship and a renewed attempt to understand the thermal and geochemical implications of the relationship.

Original languageEnglish (US)
Pages (from-to)248-251
Number of pages4
JournalGeophysical Research Letters
Volume14
Issue number3
DOIs
StatePublished - Jan 1 1987

Fingerprint

heat production
thermal structure
heat flow
heat
terrane
crust
continents
heat transmission
modeling
Antarctic regions
continent
crusts
distribution
Antarctica
province

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

Cite this

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Introduction : Background and implications of the linear heat flow‐heat production relationship. / Morgan, Paul; Sawka, Wayne N.; Furlong, Kevin Patrick.

In: Geophysical Research Letters, Vol. 14, No. 3, 01.01.1987, p. 248-251.

Research output: Contribution to journalArticle

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