Download CRC Handbook of Seafloor Heat Flow eBook
by James A. Wright,Keith E. Louden
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Heat flow through the deep sea floor History of ocean basins In Wright, J. and Louden, K. E. (ed., CRC Handbook of Seafloor Heat Flow. Boca Raton: CRC Press, pp. 3–72.
Heat flow through the deep sea floor. Advances in Geophysics, 3, 153–181. CrossRefGoogle Scholar. Carlson, R. and Johnson, H. 1994. History of ocean basins. In Engel, A. James, H. and Leonard, B. F., Petrologic Studies. Boulder: Geological Society of America, Vol. 4, pp. 599–620. Subsidence of ‘normal’ seafloor: Observations do indicate ‘flattening’. In Wright, J. Marty, J. and Cazenave, . 1989. Regional variations in subsidence rate of oceanic plates: a global analysis.
Heat flow calculated with this gradient and a mean thermal conductivity of . W/(m·K) was 70 mW/m2, which is consistent with earlier . Handbook of Seafloor Heat Flow. W/(m·K) was 70 mW/m2, which is consistent with earlier geothermal data from the same area. CRC Press, In. Boca Raton. Duchkov et a. Russian Geology and Geophysics 50 (2009) 131–135.
It is sometimes nicknamed the "Rubber Bible" or the "Rubber Book", as CRC originally stood for "Chemical Rubber Company".
Conductive heat flux. History of observations Pioneering measurements of temperature below the seafloor (. The heat flow per unit area diffusing by conduction along a thermal gradient, determined as the product of the thermal gradient and thermal conductivity. Petterson, 1949; Revelle and Maxwell, 1952; Bullard, 1954) were made to compare the thermal state of the ocean crust with that of continents and thus to improve the knowledge of the present-day heat loss from the Earth.
Variations in sea-floor depth and heat flow with age provide the main constraints on the thermal structure and evolution of the oceanic lithosphere. Joint fitting of heat flow and bathymetry yields a model with a hotter, thinner lithosphere than in previous models. The new model provides a significantly better fit to the data, including those from older lithosphere previously treated as anomalous. This will facilitate the analysis of lithospheric processes, including the effects of mid-plate volcanism and swells, regional subsidence, and hydrothermal circulation near spreading centres.
We also study seafloor fluid discharge, groundwater flow and the past ground surface temperature history through . Yamano, M and S. Uyeda, Heat flow in the western Pacific, in "Handbook of Seafloor Heat Flow", J. A. Wright and K. Louden (ed., CRC Press, 1989.
We also study seafloor fluid discharge, groundwater flow and the past ground surface temperature history through high-precision and long-term temperature measurements in marine sediments and land boreholes.
CRC handbook of seafloor heat flow. Wright JA, Louden KE, Ed. Systematic heat flow measurements across the Wagner Basin, northern Gulf of California. Boca Raton, Fl. CRC Press. Segment-scale and intrasegment lithospheric thickness and melt variations near the Andrew Bain megatransform fault and Marion hot spot: Southwest Indian Ridge, 2. degrees E-35 degrees E.
The lirst reported heat flow meas-urements were made in oceanic lithosphere by Revelle and Maxwell and in the continental lithosphereby Benfield and Bullard.