Parallel computing of multi-scale continental deformation in the western united states: preliminary results | |
Liu, Mian; Yang, Youqing; Li, Qingsong; Zhang, Huai | |
刊名 | Physics of the earth and planetary interiors |
2007-08-15 | |
卷号 | 163期号:1-4页码:35-51 |
关键词 | Parallel computing Continental tectonics Finite elements San andreas fault Western us Cyberinfrastructure |
ISSN号 | 0031-9201 |
DOI | 10.1016/j.pepi.2007.06.008 |
通讯作者 | Yang, youqing(yanyo@missouri.edu) |
英文摘要 | Lithospheric deformation in the western united states is one of the best examples of diffuse continental tectonics that deviate from the plate tectonics paradigm. conceptually, diffuse continental deformation is known to result from (1) weak and heterogeneous rheology of continents and (2) driving forces that arise from plate boundaries as well as within the continental lithosphere. however, the dynamic interplay of continental rheology and driving forces, hence the geodynamics of continental tectonics, remains poorly understood. the heterogeneous rheology and multiple driving forces cause continents to deform over different spatiotemporal scales with different physical processes, yet most geodynamic models for continental tectonic avoid dealing with such multiphysics partly because of (1) the limited observational constraints of lithospheric structure and deformation, and (2) high demands on computing alaorithms and resources. these constraints, however, have relaxed significantly in recent years to permit exploration of some of the multi-scale physics governing continental tectonics. here we present preliminary results of modeling multi-scale tectonics in the western united states using parallel finite element computation. in a 3d subcontinental-scale model, we used fine numerical meshes to incorporate all major tectonic boundaries and rheological heterogeneities in the model to explore their interplay with tectonic driving forces in controlling active tectonics in the western us. in another model for the entire san andreas fault system, we explored strain localization and simulated fault behavior at multi-timescales ranging from rupture in seconds to secular fault creep in tens of thousands of years. these models can help to integrate data grids with distributed high-performance computing resources in the emerging geosciences cyberinfrastructure. (c) 2007 elsevier b.v. all rights reserved. |
WOS关键词 | CALIFORNIA SHEAR ZONE ; NORTH-AMERICA PLATE ; SAN-ANDREAS FAULT ; GLOBAL POSITIONING SYSTEM ; BASE-LINE INTERFEROMETRY ; SOUTHERN SIERRA-NEVADA ; RANGE PROVINCE ; STRAIN ACCUMULATION ; SUBDUCTION ZONE ; SPACE GEODESY |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000249483200004 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/2380009 |
专题 | 中国科学院大学 |
通讯作者 | Yang, Youqing |
作者单位 | 1.Univ Missouri, Dept Geol Sci, Columbia, MO 65211 USA 2.Lunar & Planetary Inst, Houston, TX 77058 USA 3.Grad Univ Chinese Acad Sci, Computat Geodynam Lab, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, Mian,Yang, Youqing,Li, Qingsong,et al. Parallel computing of multi-scale continental deformation in the western united states: preliminary results[J]. Physics of the earth and planetary interiors,2007,163(1-4):35-51. |
APA | Liu, Mian,Yang, Youqing,Li, Qingsong,&Zhang, Huai.(2007).Parallel computing of multi-scale continental deformation in the western united states: preliminary results.Physics of the earth and planetary interiors,163(1-4),35-51. |
MLA | Liu, Mian,et al."Parallel computing of multi-scale continental deformation in the western united states: preliminary results".Physics of the earth and planetary interiors 163.1-4(2007):35-51. |
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