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TPV5
TPV205 |
|
Spontaneous rupture on a vertical strike-slip fault
in a homogeneous halfspace. There are slightly heterogeneous initial stress conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
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| TPV6 |
|
Spontaneous rupture on a vertical
strike-slip fault in a bimaterial halfspace, with high shear modulus
contrast across the fault (a "well-posed" problem).
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
fault surface.
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| TPV7 |
|
Spontaneous rupture on a vertical
strike-slip fault in a bimaterial halfspace, with low shear modulus
contrast across the fault.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
fault surface.
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| TPV8 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous halfspace. Initial stress conditions
are linearly dependent on depth. Subshear rupture conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
|
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| TPV9 |
|
Spontaneous rupture on a vertical
dip-slip fault in a homogeneous halfspace. Initial stress conditions are
linearly dependent on depth. Subshear rupture conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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TPV10
TPV210 |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Initial
stress conditions are linearly dependent on depth. Subshear rupture
conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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TPV10-2D
TPV210-2D |
|
Two-dimensional version of TPV10 and TPV210.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
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| TPV11 |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Initial
stress conditions are linearly dependent on depth. Supershear rupture
conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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| TPV11-2D |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Initial
stress conditions are linearly dependent on depth. Supershear rupture
conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
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| TPV12 |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Material
properties are linear elastic. Initial stress conditions are dependent on
depth. Strongly supershear rupture conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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| TPV12-2D |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Material
properties are linear elastic. Initial stress conditions are dependent on
depth. Strongly supershear rupture conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
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| TPV13 |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Material
properties are non-associative Drucker-Prager plastic with yielding in
shear. Initial stress conditions are dependent on depth. Strongly
supershear rupture conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
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| TPV13-2D |
|
Spontaneous rupture on a 60 degree
dipping dip-slip fault (normal fault) in a homogeneous halfspace. Material
properties are non-associative Drucker-Prager plastic with yielding in
shear. Initial stress conditions are dependent on depth. Strongly
supershear rupture conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
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|
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| TPV14 |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space. Material properties and initial stresses are
similar to TPV5.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
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|
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| TPV14-2D |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space. Material properties and initial stresses are
similar to TPV5.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
|
|
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| TPV15 |
|
Spontaneous rupture on a
left-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space. Material properties and initial stresses are
similar to TPV5.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
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|
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| TPV15-2D |
|
Spontaneous rupture on a
left-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space. Material properties and initial stresses are
similar to TPV5.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
|
|
|
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| TPV16 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous halfspace. There are randomly-generated
heterogeneous initial stress conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV17 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous halfspace. There are randomly-generated
heterogeneous initial stress conditions.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
|
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| TPV18 |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
|
|
|
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| TPV19 |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are Drucker-Prager plastic material properties in
a homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
|
|
|
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| TPV20 |
|
Spontaneous rupture on a
left-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
|
|
|
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| TPV21 |
|
Spontaneous rupture on a
left-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are Drucker-Prager plastic material properties in
a homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
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|
|
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| TPV22 |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a rightward stepover
(extensional step). There are linear elastic material properties in a
homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface #1.
Metrics for
fault surface #2.
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|
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| TPV23 |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a leftward stepover
(compressional step). There are linear elastic material properties in a
homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface #1.
Metrics for
fault surface #2.
|
|
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| TPV24 |
|
Spontaneous rupture on a
right-lateral, vertical, strike-slip fault with a rightward branch forming a 30
degree angle. There are linear elastic material properties in a homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface. |
|
|
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| TPV25 |
|
Spontaneous rupture on a
left-lateral, vertical, strike-slip fault with a rightward branch forming
a 30 degree angle. There are linear elastic material properties in a
homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
main fault surface.
Metrics for
branch fault surface.
|
|
|
|
| TPV26 |
|
Spontaneous rupture on a vertical
strike-slip fault. There are linear elastic material properties in a
homogeneous half-space. This is the linear elastic version of TPV27.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV26v2 |
|
Spontaneous rupture on a vertical
strike-slip fault. There are linear elastic material properties in a
homogeneous half-space. This is the same as TPV26 but with more-distant off-fault stations and longer running time.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV27 |
|
Spontaneous rupture on a vertical
strike-slip fault. There are Drucker-Prager viscoplastic material
properties in a homogeneous half-space.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV27v2 |
|
Spontaneous rupture on a vertical
strike-slip fault. There are Drucker-Prager viscoplastic material
properties in a homogeneous half-space. This is the same as TPV27 but with more-distant off-fault stations and longer running time.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
|
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| TPV28 |
|
Spontaneous rupture on a
non-planar vertical strike-slip fault. The fault is a vertical plane,
except for two hills. Initial shear and normal stresses on the fault are
obtained by resolving a regional stress tensor onto the fault surface.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
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| TPV29 |
|
Spontaneous
rupture on a vertical strike-slip fault with stochastic roughness. There
are linear elastic material properties in a homogeneous half-space.
Initial shear and normal stresses on the fault are obtained by resolving a
regional stress tensor onto the fault surface. This is the linear elastic
version of TPV30.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
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| TPV30 |
|
Spontaneous rupture
on a vertical strike-slip fault with stochastic roughness. There are
Drucker-Prager viscoplastic material properties in a homogeneous
half-space. Initial shear and normal stresses on the fault are obtained by
resolving a regional stress tensor onto the fault surface.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
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| TPV31 |
|
Spontaneous rupture
on a vertical strike-slip fault. There is a discontinuous 1D velocity
structure in a linear elastic half-space. Initial stresses are
proportional to the shear modulus.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV32 |
|
Spontaneous rupture
on a vertical strike-slip fault. There is a continuous 1D velocity
structure in a linear elastic half-space. Initial stresses are
proportional to the shear modulus.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV33 |
|
Spontaneous rupture on a
vertical strike-slip fault. There is a 3D velocity structure with a
low-velocity fault zone
in a linear elastic half-space. Initial shear stresses are
tapered so that the rupture stops spontaneously before reaching the
earth's surface or any edge of the fault.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
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| TPV34 |
|
Imperial Fault, Model 1. Spontaneous rupture on a
vertical strike-slip fault. There is a 3D velocity structure
in a linear elastic half-space. The velocity structure is derived from
SCEC Community Velocity Model CVM-H in the vicinity of the Imperial Fault. Initial shear and normal stresses are
proportional to the shear modulus.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
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|
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| TPV35 |
|
Parkfield 2004 M6
Earthquake.Model. Spontaneous rupture on a
vertical strike-slip fault. There is a bi-material 1D velocity structure
in a linear elastic half-space. Model parameters and initial conditions
are from the Parkfield spontaneous rupture model given in Ma et al.
2008.
Metrics that include modeling results only:
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
Metrics that include both modeling results and seismic data:
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
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|
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| TPV36 |
|
Spontaneous rupture on a 15 degree
dipping thrust fault in a homogeneous halfspace. Material
properties are linear elastic. Initial stress conditions are linearly dependent on
depth. The rupture reaches the Earth's surface.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
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| TPV37 |
|
Spontaneous rupture on a 15 degree
dipping thrust fault in a homogeneous halfspace. Material
properties are linear elastic. Initial stress conditions are linearly dependent on
depth. The rupture stops spontaneously before it reaches the Earth's surface.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
|
| TPV101 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous fullspace. Rate-state friction, using
an ageing law.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
|
| TPV102 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous halfspace. Rate-state friction, using
an ageing law.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
|
| TPV103 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous fullspace. Rate-state friction, using a
slip law with strong rate-weakening.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
|
| TPV104 |
|
Spontaneous rupture on a vertical
strike-slip fault in a homogeneous halfspace. Rate-state friction, using a
slip law with strong rate-weakening.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
|
| TPV105-2D |
|
Spontaneous rupture on a
strike-slip fault. Thermal pressurization, with rate-state friction, using
a slip law with strong rate-weakening. This is a 2D benchmark.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
|
|
|
|
| TPV105-3D |
|
Spontaneous rupture on a
strike-slip fault. Thermal pressurization, with rate-state friction, using
a slip law with strong rate-weakening. This is a 3D benchmark.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
Metrics for
fault surface.
|
|
|
|
| TPV205-2D |
|
Two-dimensional version of TPV5 and TPV205.
Metrics for
on-fault stations, organized by user.
Metrics for
on-fault stations, organized by station.
Metrics for
off-fault stations, organized by user.
Metrics for
off-fault stations, organized by station.
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