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• W2463674911 abstract "A comprehensive understanding of the thermal properties beneath the CentralRange of Taiwan is essential to decipher the process of mountain building and interpretthe observed geophysical features, such as seismic velocity and seismicity. A first-order-approximation thermal model based on crustal thickening followed by constanterosion processes is described for the Central Range. The effect of groundwater circulationon the observed surface heat flow has been excluded in our evaluation. Ourresults indicate that crustal thickening causes a decrease in the geothermal gradientand the temperature. Erosion causes an increase in the geothermal gradient and thetemperature. Through modeling, we derived the optimum geotherm below the CentralRange by considering a thickening factor of 2 for crustal thickening occurring at 10Ma following constant erosion since 5 Ma. The preferred final geotherm estimated amoderate geothermal gradient of ~17 °C/km and a temperature of ~210-550 °C ata depth of 10-30 km. The uncertainties in the thickening factor, the time of crustalthickening, and the prethickening crustal thickness have a temperature-differenceeffect of only a few tens of degrees compared to the temperature yielded by the preferredfinal geotherm. Other geotherm parameters such as radiogenic heat flow, scaledepth, 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 QPvalues set limits on the middle- and lower-crust temperatures determined by ourmodel. The resulting moderate geothermal gradient differs from the notion that thecrust beneath the Central Range is hot, although the temperature in the shallowcrust needs further investigation." @default.
• W2463674911 created "2016-07-22" @default.
• W2463674911 creator A5002796845 @default.
• W2463674911 creator A5014658952 @default.
• W2463674911 date "2002-01-01" @default.
• W2463674911 modified "2023-10-16" @default.
• W2463674911 title "Estimation of the thermal structure of a young orogenic belt according to a model of whole-crust thickening" @default.
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• W2463674911 doi "https://doi.org/10.1130/0-8137-2358-2.121" @default.
• W2463674911 hasPublicationYear "2002" @default.
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