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- W2049113068 abstract "The amount and distribution of residual thermoluminescence in limestone contact zones is theoretically calculated by numerically integrating the appropriate thermal-decay equations over the time and temperature conditions predicted by heat-conduction theory. The resultant thermoluminescence pattern is best characterized by the relative width of the zone of complete thermoluminescence annealing. Based on this feature, a method of determining magma temperature is developed and analyzed. Effective magma temperatures of 950° C. are inferred from the natural thermoluminescence in limestone wall rock in association with late Pleistocene basaltic flows and dikes in northern Arizona." @default.
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- W2049113068 date "1966-09-01" @default.
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- W2049113068 title "Geothermometry from the Thermoluminescence of Contact-Metamorphosed Limestone" @default.
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- W2049113068 doi "https://doi.org/10.1086/627192" @default.
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