TriBIE is a parallelized Fortran90 (OpenMPI) code for simulating episodic slow slip events (SSEs) and earthquake cycles in an arbitrary curved fault buried in half-space medium. The quasi-dynamic formulation of shear traction and fault slip [Rice 1993] is implemented in spatial domain and the 5th-order Runge-Kutta method with adaptive time step integration is used in time domain. TriBIE has been used in many geophysical applications recently. TriBIE has also been verified in the SCEC Sequences of Earthquakes and Aseismic Slip Project (https://strike.scec.org/cvws/seas/).
TriBIE is developed and currently maintaned by Duo Li (https://daisy20170101.github.io/duo_li.github.io/), Yajing Liu(https://www.mcgill.ca/eps/liu), Hongyu Yu, Lei Zhang and Andrea Perez-Silva (). Please feel free to contact us for anything about the code!
Figure 1. Numerical model of the curved subduction fault in Cascadia (left) and the simulated SSE slip in two episodes [Li and Liu, 2016; 2017].
We use analytical solution for stress tensor in polygon elements embeded in homogeneous half-space.
We can use pylith to calculate stiffness for triangular elements in 3D curved slab geometry with either 1D or 3D velocity.
$ mpiifort src/phy3d_module_non.f90 src/3dtriBIE_v1.f90 -o 3dtriBIE
Line 1: jobname (appendix)
Line 2: foldername
Line 3: stiffname
Line 4: restartname
Line 5: profile
Line 6: Number of points in a-b profile, total element,element/process,num. of procs,h*
Line 7: Idin,Idout,Iprofile,Iperb,Isnapshot
Line 8: factor1,factor2,factor3,factor4
Line 9: Vpl in mm/yr
Line 10: up-limit of locking depth, bottom-limit of locking depth
Line 11: \bar{sigma} in locking depth, \bar{sigma} in SSE,d_c in SSE depth
Line 12: simulation time in year
Line 13: tslip_ave,tslip_aveint
Line 14: tint_out,tmin_out,tint_cos
Line 15: vcos,vsse1,vsse2
Line 16: tssestart,tsseend
Line 17: nmv,nas,ncos,nsse
Line 18: s1,s2,s3,s4,s5,s6,s7,s8
Example:
-test.dat
./out/
../Code1/TriGreen/
./out/out0-test.dat
../Code1/profiles/GuerreroT.dat
5 90496 1414 64 122 !Nab,Nt_all,Nt,nprocs,hnucl
1 1 2 1 0 !Idin, Idout Iprofile, Iperb,Isnapshot
2.0 0.98 1.03 1.0 ! (factor1 factor2 factor3 factor4)
61.0 ! Vpl (mm/yr)
20.0 45.0 !xilock1 xilock2 (SSE depth)
500.0 25.0 10.0862 !sigmadiff, sefffix (bar), Lffix (mm)
200.0 ! tmax
0.0 5.0 !tslip_ave tslip_aveint
100.0 1.0 1.585d-8 !tint_out tmin_out tint_cos (3.17d-8 is 1sec)
5.0 61.0 305.0 !vcos (mm/s), vsse1(3Vpl) vsse2 (5Vpl, mm/yr)
0.0 2000.0 ! sse start and end times to record moment
500 30 30 30 ! nmv,nas,ncos,nsse
72081 15189 5372 4900 3138 65037 18071 20293 ! output element IDs (s1-s8)
Jiang, J., B. Erickson, V. Lambert, J.-P. Ampuero, R. Ando, S. Barbot, C. Cattania, L. D. Zilio, B. Duan, E. M. D. . and et al. "Community-Driven Code Comparisons for Three-Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip (SEAS)." JGR: Solid Earth
Perez-Silva, A., D. Li, A.-A. Gabriel and Y. Kaneko (2021). "3D Modeling of Long-Term Slow Slip Events Along the Flat-Slab Segment in the Guerrero Seismic Gap, Mexico." Geophysical Research Letters 48(13).
Perez-Silva, A., Y. Kaneko, M. Savage, L. Wallace, D. Li and C. Williams (2022). "Segmentation of Shallow Slow Slip Events at the Hikurangi Subduction Zone Explained by Along-Strike Changes in Fault Geometry and Plate Convergence Rates." Journal of Geophysical Research: Solid Earth 127(1): e2021JB022913.
Li, H., M. Wei, D. Li, Y. Liu, Y. Kim and S. Zhou "Segmentation of Slow Slip Events in South Central Alaska Possibly Controlled by a Subducted Oceanic Plateau." Journal of Geophysical Research: Solid Earth.
H Yu, Y Liu, H Yang, J Ning , Modeling earthquake sequences along the Manila subduction zone: Effects of three-dimensional fault geometry. Tectonophysics, 2018
Li, D. and Y. Liu (2016). "Spatiotemporal evolution of slow slip events in a nonplanar fault model for northern Cascadia subduction zone." Journal of Geophysical Research: Solid Earth 121(9): 6828-6845.
Li, D. and Y. Liu (2017). "Modeling slow-slip segmentation in Cascadia subduction zone constrained by tremor locations and gravity anomalies." Journal of Geophysical Research: Solid Earth 122: 3138–3157.