New heat flow observations on the Reykjanes Ridge

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K. Bram

Abstract

During METEOR cruise 45 in August 1977 14 heat flow measurements were obtained along a profile east of the Reykjanes Ridge and perpendicular to the ridge axis covering a distance range from 30 to 240 km. Closely spaced measurements were grouped together. The mean heat flow of all groups amounts to 109±20 mW m-2. The values do not reveal a distinct increase with decreasing distance from the ridge axis as may be expected from the theoretical heat flow distribution based upon a cooling plate model. Including earlier measurements a high and very uniform heat flow in the distance range from 170 to 340 km was observed with a mean value of about 100 mW m-2. In order to explain this high heat flow a temperature of 930° C is required at the lower boundary of the lithosphere at a depth of 50 km, assuming a purely conductive heat transport. Compared with the results obtained from previous measurements west of the Reykjanes Ridge, the data reveal an asymmetric thermal behaviour of the ridge area. The average heat flow east of the ridge amounts to 93 mW m-2 being nearly twice the heat flow of the region west of the ridge.


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How to Cite
Bram, K. (1980). New heat flow observations on the Reykjanes Ridge. Journal of Geophysics, 47(1), 86-90. Retrieved from https://journal.geophysicsjournal.com/JofG/article/view/37

References

Beblo, M., Bjornsson, A. (1978) Magnetotelluric investigations of the lower crust and upper mantle beneath Iceland. J. Geophys. 45:1-16

Elder, J.W. (1965) Physical processes in geothermal areas. In. Terrestrial heat flow, W.H.K. Lee, ed. Washington D.C. Geophys. Monogr. Am. Geophys. Union 8:211-237

Fleischer, U. (1974) The Reykjanes Ridge - a summary of geophysical data. In: Geodynamics of Iceland and the North Atlantic Area, L. Kristjansson (Ed.) 17-31, Dordrecht. D. Reidel

Hanel, R. (1972) Heat flow measurements in the Ionian Sea with a new heat flow probe. Meteor Forschungsergeb. Reihe C: 11:105-108

Herzen, R.P. Von, Maxwell, E.A. (1959) The measurement of thermal conductivity of deep sea sediments by a needle-probe method. J. Geophys. Res. 64:1557-1565

Herzen, R.P. Von, Lee, W.H.K. (1969) Heat flow in oceanic regions. In: The Earth's Crust and Upper Mantle, P.J. Hart (Ed.) Washington D.C. Geophys. Monogr. Am Geophys. Union 13:88-95

Jones, E.J.W., Ewing, M., Ewing, J.I., Eittreim, S.L. (1970) Influences of Norwegian Sea overflow water on sedimentation in the northern North Atlantic and Labrador Sea. J. Geophys. Res. 75:1655-1680

Kappelmeyer, 0., Hanel, R. (1974) Geothermics with special reference to application. Geoexploration Monographs, Ser. I, No. 4, p.238. Berlin: Gebr. Borntrager

Langseth, M.G., Zielinski, G.W. (1974) Marine heat flow measurements in the Norwegian-Greenland sea and in the vicinity of Iceland. In: Geodynamics of Iceland and the North Atlantic Area, L. Kristjansson (Ed.) pp. 277-295. Dordrecht: D. Reidel

Lee, W.H.K., Uyeda, S. (1965) Review of heat flow data. In: Terrestrial heat flow. W.J.K. Lee (Ed.) Washington D.C. Geophys. Monogr Am. Geophys. Union 8:87-190

Lister, C.R.B. (1972) On the thermal balance of a mid-ocean ridge. Geophys. J.Roy. Astron. Soc. 26:515-535

McKenzie, D.P. (1967) Some remarks on heat flow and gravity anomalies. J. Geophys. Res. 72:6261-6273

Palmason, G. (1967) On heat flow in Iceland in relation to the mid-Atlantic ridge. In Iceland and Mid-Ocean-Ridges, S. Bji:irnsson, ed. Soc. Sci. lsi. 38:lll-127

Parker, R.L., Oldenburg, D.W. (1973) Thermal model of ocean ridges. Nature Phys. Sci. 242:137-139

Parsons, B., Sclater, J.G. (1977) An analyses of the variation of ocean floor bathymetry and heat flow with age. J. Geophys. Res. 82:803-827

Sclater, J.G., Crowe, J., Anderson, R.N. (1976) On the reliability of oceanic heat flow measurements. J. Geophys. Res. 81:2997-3006

Sclater, J.G., Crowe, J. (1979) A heat flow survey at anomaly 13 on the Reykjanes Ridge: a critical test of the relation between heat flow and age. J. Geophys. Res. 84:1593-1602

Sclater, J.G., Herzen, R.P. Von, Williams, D.L., Anderson, R.N., Klitgord, K. (1974) The Galapagos spreading center, heat flow low on the north flank. Geophys. J. Roy. Astron. Soc. 38:609-626

Scheljagin, W.A., Buatschidse, J.M., Buatschidse, G.J., Schoar, M.P. (1973) In: Catalogue of data (3) Moscow: Soviet Geophysical Committee of the Academy of Sciences of the USSR

Schilling, J.G. (1973) Iceland mantle plume: geochemical study of Reykjanes ridge. Nature 242:565-571

Talwani, M., Windisch, C.C., Langseth, M.G. (1971) Reykjanes Ridge crest: a detailed geophysical study. J. Geophys. Res. 76:473-517

Vine, F.J. (1966) Spreading of the ocean floor· new evidence. Science 15:1405-1515

Vogt, P.R. (1971) Asthenosphere motion recorded by the ocean floor south of Iceland. Earth Planet. Sci. Lett. 13:153-160

Vogt, P.R., Johnson, G.L. (1973) A longitudinal seismic reflection profile of the Reykjanes Ridge: Part !-Evidence for west-flowing bottom water. Earth Planet Sci. Lett. 18:45-48

Williams, D.L., Herzen, R.P. Von, Sclater, J.G., Anderson, R.N. (1974) The Galapagos spreading center: lithospheric cooling and hydrothermal circulation. Geophys. J. Roy. Astron. Soc. 38:587-608

Worthington, LV., Volkmann, G.H. (1965) The volume transport of the Norwegian Sea overflow water in the North Atlantic. Deep-Sea Res. 12:667-676