Abstract

Ascertaining regional radiogeochemical characteristics and lithospheric thermal structure characteristics is paramount for identifying the resource potential of hot dry rocks (HDRs). This study conducted thermal conductivity testing and whole-rock analyses of outcrop granites of different formation epochs from the Tengchong area. Moreover, combined with the previously published whole-rock data and the data related to radioactive heat production rates, this study conducted geological, geophysical, and geothermal analyses. Key findings are as follows: (1) Granites in the Tengchong area exhibit an average radioactive heat generation rate of 5.54 μW/m 3 . Among them, the Late Cretaceous granites have an average radioactive heat generation rate of 8.08 μW/m 3 , suggesting high heat production granites; (2) Granites in the Tengchong area present an average thermal conductivity of 3.135 W/(m·K), relatively akin to the average values of granitic rocks worldwide. Compared to granites of other epochs, the Late Cretaceous granites manifest significantly higher thermal conductivities, with an average of 3.28 W/(m·K); (3) There is a negative correlation between the mica content and the thermal conductivity of the granites in the Tengchong area; (4)The Tengchong area holds potential for HDR exploitation and is inferred to have a lithospheric structure characterized by hot mantle and cold crust.

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