Estimation of the thermal structure of a young orogenic belt according to a model of whole-crust thickening

Abstract

A comprehensive understanding of the thermal properties beneath the Central Range of Taiwan is essential to decipher the process of mountain building and interpret the observed geophysical features, such as seismic velocity and seismicity. A first-order-approximation thermal model based on crustal thickening followed by constant erosion processes is described for the Central Range. The effect of groundwater circulation on the observed surface heat flow has been excluded in our evaluation. Our results indicate that crustal thickening causes a decrease in the geothermal gradient and the temperature. Erosion causes an increase in the geothermal gradient and the temperature. Through modeling, we derived the optimum geotherm below the Central Range by considering a thickening factor of 2 for crustal thickening occurring at 10 Ma following constant erosion since 5 Ma. The preferred final geotherm estimated a moderate geothermal gradient of ~17 °C/km and a temperature of ~210-550 °C at a depth of 10-30 km. The uncertainties in the thickening factor, the time of crustal thickening, and the prethickening crustal thickness have a temperature-difference effect of only a few tens of degrees compared to the temperature yielded by the preferred final geotherm. Other geotherm parameters such as radiogenic heat flow, scale depth, and surface heat production are also tested in the final geotherm calculations. Seismicity cutoff depth (i.e., the brittle-to-ductile transition depth) and seismic QP values set limits on the middle- and lower-crust temperatures determined by our model. The resulting moderate geothermal gradient differs from the notion that the crust beneath the Central Range is "hot," although the temperature in the shallow crust needs further investigation.

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