ASPECT parameter files for building stress field of Korea Peninsula.

# ----------------------------------------------------------------------# Sungho Lee# SEISMOLOGICAL LABORATORY, Seoul National University, South Korea# [e-mail] or [e-mail]# Thses input files were used for aspect in my reasearch project# The publication title is "Contribution of viscous flow driven by upper mantle heterogeneities to upper crustal seismicity in the Korean Peninsula" (in preparation, July./2021)# ----------------------------------------------------------------------<br>#### ASPECT input files ##### Case0.prm, Layered crustal model (upper crust: 20 km, lower crust: 10 km) and laterally uniform temperature.# Case1.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km)# Chemical composition of mantle follows average of harzburgite and lherzolite# It is conincidence with Case 2-1 in the manuscript# Case2.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (50 MPa)# Chemical composition of mantle follows average of harzburgite and lherzolite# It is conincidence with Case 2-2 in the manuscript# Case3.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (100 MPa)# Chemical composition of mantle follows average of harzburgite and lherzolite# It is conincidence with Case 2-3 in the manuscript# Case4.prm, crustal thikcness variation with laterally uniform temperature# It is conincidence with Case 1-1 in the manuscript# Case5.prm, crustal thikcness variation with laterally uniform temperature with traction boundary condition on the western side wall (50 MPa)# It is conincidence with Case 1-2 in the manuscript# Case6.prm, crustal thikcness variation with laterally uniform temperature with traction boundary condition on the western side wall (100 MPa)# It is conincidence with Case 1-3 in the manuscript# Case7.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (50 MPa)# Chemical composition of mantle follows harzburgite# Case8.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (50 MPa)# Chemical composition of mantle follows lherzolite<br>#### data dir. ##### crustal_isostacy.txt, intial guess for topography resulted from Case 1-1. The guess was used for reducing simulation time# initial_material.txt, composition model for upper and lower cursts and mantle which is from CRUST1.0 data# initial_temperature_Vs_FWEA18.txt, initial temperature for Case 1 to Case 3# initial_temperature_1d_geotherm.txt, initial temperature for Case 4 to Case 6# initial_temperature_Vs_FWEA18_harzburgite.txt, initial temperature for Case 7# initial_temperature_Vs_FWEA18_lherzolite.txt, initial temperature for Case 8<br>#### traction dir. ##### traction_case2.txt, traction data for Case 2# traction_case3.txt, traction data for Case 3# traction_case5.txt, traction data for Case 5# traction_case6.txt, traction data for Case 6# traction_case7.txt, traction data for Case 7# traction_case8.txt, traction data for Case 8