The chapter reviews heat generation in crystalline rocks and influences on overlying sedimentary basins in western australia wa. The heat generation is determined from the half life of the isotopes in the material as well as their decay types. A mean heat flow density value of 40 l s d mw m 2 for the three boreholes of the hyderabad granitic region is obtained radioactive heat generationdata on the concentration of radioactive elements u th k as obtained from measurements on 29 samples of granite from the hyderabad region is available padmakumari et al 1977.
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