A heat production model of a shield area and its implications for the heat flow ‐ Heat production relationship

David M. Fountain, Kevin Patrick Furlong, Matthew H. Salisbury

Research output: Contribution to journalArticle

18 Citations (Scopus)

Abstract

The Pikwitonei and Sachigo subprovinces of central Manitoba provide a cross‐sectional view of the Superior Province Crust. To constrain thermal models of the crust, we measured heat production and thermal conductivity in rocks from this terrain using standard gamma‐ray spectrometry and divided bar techniques. These data, when used in a two‐dimensional model of shield crust, show that estimates of surface heat flow and surface heat production yield the well‐known linear relationship between surface heat production and surface heat flow observed for heat flow provinces. This demonstrates that determinations of heat production with depth based on inversion of the linear heat production‐heat flow relationship are non‐unique.

Original languageEnglish (US)
Pages (from-to)283-286
Number of pages4
JournalGeophysical Research Letters
Volume14
Issue number3
DOIs
StatePublished - Jan 1 1987

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heat production
heat transmission
heat flow
shield
heat
crusts
crust
Manitoba
bedrock
thermal conductivity
spectrometry
rocks
inversions
conductivity
estimates
rock
spectroscopy
province

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

Cite this

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A heat production model of a shield area and its implications for the heat flow ‐ Heat production relationship. / Fountain, David M.; Furlong, Kevin Patrick; Salisbury, Matthew H.

In: Geophysical Research Letters, Vol. 14, No. 3, 01.01.1987, p. 283-286.

Research output: Contribution to journalArticle

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