DOIAbstract
An apparatus to measure heat flow through the ocean floor in con-junction with standard coring techniques has been independently developed at Cambridge. Experimental and theoretical work have shown that the probe configuration used is free from systematic error in the temperature measurement due to heat generated by fric-tion when the device enters the sediment. A number of successful heat flow measurements and temperature/depth profiles in the sea have been obtained: summarized data on these is presented. I
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