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

Keyphrases

• Thermal Structure 100%
• Orogenic Belt 100%
• Geotherm 100%
• Crustal Thickening 100%
• Central Range 80%
• Geothermal Gradient 80%
• Thickening Factor 40%
• Taiwan 20%
• Seismicity 20%
• Erosion Mechanism 20%
• Geophysical Characteristics 20%
• Seismic Velocity 20%
• Heat Flow 20%
• Thermal Properties 20%
• Lower Crust 20%
• Mountain Building 20%
• Groundwater Circulation 20%
• Flow Scales 20%
• Seismicity Cut-off 20%
• Thermal Model 20%
• Heat Production 20%
• Middle Crust 20%
• Surface Heat Flow 20%
• Brittle-ductile Transition 20%
• Transition Depth 20%
• Temperature Difference Effect 20%
• Shallow Crust 20%
• Radiogenic Heat 20%
• Crustal Thickness 20%

Earth and Planetary Sciences

• Thermal Structure 100%
• Crustal Thickening 100%
• Geothermal Gradient 100%
• Orogenic Belt 100%
• Seismicity 50%
• Taiwan 25%
• Seismic Velocity 25%
• Lower Crust 25%
• Mountain Building 25%
• Heat Production 25%
• Crustal Thickness 25%
• Groundwater Circulation 25%