2008-汶川8.0级大地震:地表破裂与震害图集 本书特色

《2008汶川8.0级大地震:地表破裂与震害图集(英文版)》由高等教育出版社出版。

2008-汶川8.0级大地震:地表破裂与震害图集 内容简介

简介 　　《2008汶川8.0级大地震:地表破裂与震害图集(英文版)》由高等教育出版社出版。

2008-汶川8.0级大地震:地表破裂与震害图集 目录

1. Tectonic Setting of the Wenchuan Earthquake2. Outline of Earthquake and Focal Mechanisms3. Outline of Co-seismic Surface Rupture3.1 Distribution of co-seismic surface rupture3.2 Slip distribution of co-seismic fault4. Deformation Characteristics of Co-seismic Surface Rupture4.1 Co-seismic fault scarp4.2 Co-seismic flexure-slip fold structure5. Relationship Between Surface Rupture and Pre-existing Active Faults 6. Relationship Between Surface Rupture and Damage to Infrastructure 7. Co-seismic Landsliding and Liquefaction8. Earthquake Disaster9. Relief OperationsReferencesIndex of Figures

2008-汶川8.0级大地震:地表破裂与震害图集 节选

《2008汶川8.0级大地震:地表破裂与震害图集(英文版)》内容简介：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 相关资料

插图：3.1 Distribution of co-seismic surface ruptureField investigations reveal that the Ms 8.0 Wenchuan earthquake of 12 May 2008 produced a 285-kin-long surface rupture zone along the Longmen Shan Thrust Belt, eastern margin of the TibetanPlateau, mainly along the pre-existing Yingxiu-Beichuan, Guanxian-Anxian, and Qingchuanfaults, which are three of the main active faults within the thrust belt.These faults define a left-stepping en echelon pattern with-10 km clearance. Co-seismic surface ruptures concentratedwithin a zone of Field investigations demonstrate that （i） the Wenchuan earthquake occurred upon pre-existingactive faults of the Longmen Shan Thrust Belt; （ii） the long rupture length and large thrustingslip resulted from compressive stress associated with eastward extrusion of the Tibet Plateau asit accom

2008-汶川8.0级大地震:地表破裂与震害图集 作者简介

Dr. Aiming Lin is Professor at Shizuoka University, Japan.

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