Computational Earthquake Physics: Simulations, Analysis and Infrastructure, Part I
Exciting developments in earthquake science have benefited from new observations, improved computational technologies, and improved modeling capabilities. Designing realistic supercomputer simulation models for the complete earthquake generation process is a grand scientific challenge due to the com...
| Συγγραφή απο Οργανισμό/Αρχή: | |
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| Άλλοι συγγραφείς: | , , , |
| Μορφή: | Ηλεκτρονική πηγή Ηλ. βιβλίο |
| Γλώσσα: | English |
| Έκδοση: |
Basel :
Birkhäuser Basel,
2006.
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| Σειρά: | Pageoph Topical Volumes
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| Θέματα: | |
| Διαθέσιμο Online: | Full Text via HEAL-Link |
Πίνακας περιεχομένων:
- Computational Earthquake Physics PART I: Introduction
- Fracture of a Liquefied Crack and the Physics of Rayleigh Waves
- Experimental Evidence of Critical Sensitivity in Catastrophe
- Implementation of Particle-scale Rotation in the 3-D Lattice Solid Model
- Numerical and Experimental Study on Progressive Failure of Marble
- 3-D Simulation of Tectonic Loading at Convergent Plate Boundary Zones: Internal Stress Fields in Northeast Japan
- Virtual California: Fault Model, Frictional Parameters, Applications
- Catastrophic Rupture Induced Damage Coalescence in Heterogeneous Brittle Media
- Differences Between Mode I and Mode II Crack Propagation
- Dynamic Rupture in a 3-D Particle-based Simulation of a Rough Planar Fault
- Numerical Simulation of the Effect of a DC Electric Field on Seismic Wave Propagation with the Pseudospectral Time Domain Method
- Quartz Rheology and Short-time-scale Crustal Instabilities
- Recurrence Interval Statistics of Cellular Automaton Seismicity Models
- Parallel 3-D Simulation of a Fault Gouge Using the Lattice Solid Model
- Benioff Strain Release Before Earthquakes in China: Accelerating or Not?
- Improvement in the Fault Boundary Conditions for a Staggered Grid Finite-difference Method
- The Displacement and Strain Field of Three-dimensional Rheologic Model of Earthquake Preparation
- Deformations in Transform Faults with Rotating Crustal Blocks
- Elasticity, Yielding and Episodicity in Simple Models of Mantle Convection.
