DOI: 10.6084/m9.figshare.13502223
title: ASPECT input files (parameters and initial and boundary conditions)

description: # ----------------------------------------------------------------------# Sungho Lee# SEISMOLOGICAL LABORATORY, Seoul National University, South Korea# sungho91@snu.ac.kr or sungho91123@gmail.com# Thses input files were used for aspect in my reasearch project# The publication title is "Origin of seismicty in the Korean Peninsula and implication for intraplate earthqaukes" (in preparation, Dec./2020)# ----------------------------------------------------------------------<br>#### ASPECT input files ##### Case1-1.prm, crustal thikcness variation with laterally uniform temperature# Case1-2.prm, crustal thikcness variation with laterally uniform temperature with traction boundary condition on the western side wall (50 MPa)# Case1-3.prm, crustal thikcness variation with laterally uniform temperature with traction boundary condition on the western side wall (100 MPa)# Case2-1.prm, lithospheric thickness variation with laterally non-uniform temperature (0 - 200 km)# Case2-2.prm, lithospheric thickness variation with laterally non-uniform temperature (0 - 200 km) with traction boundary condition on the western side wall (50 MPa)# Case2-3.prm, lithospheric thickness variation with laterally non-uniform temperature (0 - 200 km) with traction boundary condition on the western side wall (100 MPa)# Case3-1.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km)# Case3-2.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (50 MPa)# Case3-3.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (100 MPa)<br>#### data dir. ##### crustal_isostacy.txt, intial guess for topography resulted from Case 1-1. The guess was used Case 1-2 to Case 3-3 for reducing simulation time# initial_material_1.txt, composition model for upper and lower cursts and mantle which is from CRUST1.0 data# initial_temperature_Vs_cr.txt, initial temperature for Case 1-1 to Case 1-3# initial_temperature_Vs_litho.txt, initial temperature for Case 2-1 to Case 2-3# initial_temperature_Vs_FWEA18.txt, initial temperature for Case 3-1 to Case 3-3<br>#### traction dir. ##### traction_case1_50.txt, traction data for Case 1-2# traction_case1_100.txt, traction data for Case 1-3# traction_case2_50.txt, traction data for Case 2-2# traction_case2_100.txt, traction data for Case 2-3# traction_case3_50.txt, traction data for Case 3-2# traction_case3_100.txt, traction data for Case 3-3<br># We uploaded additional files for different mineral compositions of mantle#### Case3-2_chemical_heterogenity dir. ####<br>#### ASPECT input files ##### Case3-2_lherzolite.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (50 MPa)# case3-2_harzburgite.prm, Full upper mantle structures with laterally non-uniform temperature (0 - 660 km) with traction boundary condition on the western side wall (50 MPa)<br>#### data dir. ##### lherzolite_isostacy.txt, intial guess of topography for Case 3-2_lherzolite.prm# harzburgite_isostacy.txt, intial guess of topography for Case 3-2_harzburgite.prm# initial_temperature_Vs_FWEA18_lherzolite.txt, initial temperature for Case 3-2_lherzolite.prm# initial_temperature_Vs_FWEA18_harzburgite.txt, initial temperature for Case 3-2_harzburgite.prm<br>#### traction dir. ##### traction_case3_50_lherzolite.txt, traction data for Case 3-2_lherzolite.prm# traction_case3_50_harzburgite.txt, traction data for Case 3-2_harzburgite.prm<br>