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- W2085362912 abstract "The participation of the USC&GSS Pioneer in the International Indian Ocean Expedition included a major geophysical investigation of the Andaman Sea during April and May of 1964. A program of heat-flow measurements was motivated by known volcanism within the basin, indications of warmer bottom water than can be explained by simple adiabatic heating, and a general lack of data on the major seismic belt that runs through the Andaman-Nicobar area from Burma into Sumatra. As part of operations in the area, four successful measurements were made of the heat flow associated with the inner or volcanic trend of the primary arc that encloses the Andaman Sea. A modified form of the thermograd [Gerard et al., 1962] was used to obtain a recording of the temperature gradient in the bottom sediment and a core, from which the coefficient of thermal conductivity of the bottom sediment can be determined. The heat flow defined here is a flow per unit area; it is determined as the product of the temperature gradient in the bottom sediment and the thermal conductivity of the sediment." @default.
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- W2085362912 date "1964-11-15" @default.
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- W2085362912 title "Sea bottom heat-flow measurements in the Andaman Sea" @default.
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- W2085362912 doi "https://doi.org/10.1029/jz069i022p04918" @default.
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