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Geothermal flow and phenomena in two Swedish localities north of the Arctic circle
1982 (English)In: Geophysical Journal International, ISSN 0956-540X, E-ISSN 1365-246X, Vol. 71, no 3, p. 545-554Article in journal (Refereed) Published
Abstract [en]

Temperature measurements in eight holes reaching vertical depths between 287 and 1100m below ground surface in the Malmberget area (lat. 67° 10' N, long. 20° 40' E Gr.) and the Kiruna area (lat. 67° 52' N, long. 20° 9' E Gr.) in the Swedish Precambrian are reported. The mean equilibrium heat flow in this part of the Swedish shield after climatic correction is 52.6 ± 1.7mWm-2. The mean uncorrected heat flow is 46.6 mWm-2. Comparison with other shield areas shows that in common with the S. African and Indian shields, the north Swedish shield has a greater heat flow than the remaining shield areas of the world.

Place, publisher, year, edition, pages
1982. Vol. 71, no 3, p. 545-554
National Category
Geophysics
Research subject
Applied Geophysics
Identifiers
URN: urn:nbn:se:ltu:diva-4157DOI: 10.1111/j.1365-246X.1982.tb02782.xISI: A1982PT69900001Scopus ID: 2-s2.0-0020430139Local ID: 20ce41c0-2beb-11dd-8657-000ea68e967bOAI: oai:DiVA.org:ltu-4157DiVA, id: diva2:977021
Note
Godkänd; 1982; 20080527 (cira)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2018-07-10Bibliographically approved

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Parasnis, Dattatray

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