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- W2051208310 abstract "Nine closely spaced heat flow observations were made near 43°N 20°W during a detailed survey of Peake and Freen deeps situated on the eastern side of the Mid-Atlantic Ridge. These values range from 1.23 to 1.76 μcal./cm2·sec and all are close to the Atlantic average of 1.34 μcal./cm2·sec. This result, together with the absence of any known earthquake epicenters, implies that there is no igneous activity in the area at present. The observed scatter in the heat flow values cannot be attributed solely to experimental error but must be partly due to environmental effects. Quantitative estimates of the effects of variations of water temperature and recent rapid sedimentation show that it is unlikely that these effects are of sufficient magnitude to explain the scatter. A numerical method is developed to compute the heat flow through a region where both irregularities in sediment thickness and topographic relief are known. It is demonstrated that the observed variation of sediment thickness and surface relief in the vicinity of the stations can explain the differences in heat flow." @default.
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- W2051208310 date "1970-09-01" @default.
- W2051208310 modified "2023-09-25" @default.
- W2051208310 title "The relationship of heat flow, bottom topography and basement relief in peake and freen deeps, Northeast Atlantic" @default.
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- W2051208310 doi "https://doi.org/10.1016/0040-1951(70)90111-3" @default.
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