The Great Wenchuan Earthquake of 2008S: A Photographic Atlas ofSurface Rupture and Related Disaster focuses on the main deformationcharacteristics of co-seismic surface rupture, including rupture length andslip distribution of co-seismic surface rupture caused by the WenchuanEarthquake and its associated relief operation. The magnitude Ms 8.0(Mw 7-9) Wenchuan Earthquake occurred on 12 May 2008 in the LongmenShah region of China, the topographical boundary between the TibetanPlateau and the Sichuan Basin, resulting in extensive damage throughoutcentral and western China. This atlas contains distinct photographs obtainedduring the field investigation carried out immediately 2 days after thequake. The atlas is designed for geologists, seismologists and architectureengineers engaged in seismic mechanisms and surface rupture deformationcharacteristics of large intracontinental earthquakes.
2008汶川8.0级大地震:地表破裂与震害图集(英文版)
2009-09
高等教育出版社
- 高等教育出版社
- 9787040151282
- 1版
- 227428
- 46246562-6
- 精装
- 16开
- 2009-09
- -
- 160
- 130
- -
- 理学
- 地质学
- 0709
- P316.271-64
- 地球科学
- 继续教育(成教、自考、函授、网络)
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Front Matter
ctonic Setting of the Wenchuan Earthquake
tline of Earthquake and Focal Mechanisms
tline of Co-seismic Surface Rupture
3.1 Distribution of co-seismic surface rupture
3.2 Slip distribution of co-seismic fault
formation Characteristics of Co-seismic Surface Rupture
4.1 Co-seismic fault scarp
4.2 Co-seismic flexure-slip fold structure
lationship Between Surface Rupture and Pre-existing Active Faults
lationship Between Surface Rupture and Damage to Infrastructure
-seismic Landsliding and Liquefaction
rthquake Disaster
lief Operations
References
Index of Figures
Appendix