New heat flow data from the immediate vicinity of the Kola super-deep borehole: Vertical variation in heat flow confirmed and attributed to advection
We present new heat flow values and other geothermal data in the upper crystalline crust in the immediate vicinity of the 12.4-km deep Kola super-deep borehole, NW Russia. Our results show a systematic vertical increase in geothermal gradient and heat flow density as deep as we could measure (1.6 km...
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Published in | Tectonophysics Vol. 401; no. 1-2; pp. 119 - 142 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
Published |
25.05.2005
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Online Access | Get full text |
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