| Titre : |
5 Years after the Wenchuan Earthquake |
| Type de document : |
texte imprimé |
| Editeur : |
London : Nature Publishing Group |
| Année de publication : |
2013 |
| Collection : |
Nature Collections |
| Importance : |
1 vol. (52 p.) |
| Présentation : |
ill., graph., fig., tabl. |
| Format : |
28 cm |
| Note générale : |
PPN 280354738
Compilation d'articles parus dans Nature Geoscience |
| Langues : |
Anglais (eng) |
| Tags : |
Séisme de Wenchuan (2008) Wenchuan Earthquake, China, 2008 |
| Index. décimale : |
551.220 951 Tremblements de terre - Chine et territoires adjacents (Tibet, Sinkiang, Mongolie, Mandchourie) |
| Résumé : |
The Wenchuan earthquake that occurred in southwest China on 12 May 2008 killed more than 80,000 people and displaced millions. Five years on, many of the affected communities have made a good recovery – at least until the most recent quake in April 2013 wreaked further havoc in the region. The devastating 2008 event has helped invigorate research into earthquake hazards. A collection of opinion pieces, published in Nature Geoscienceto mark the fifth anniversary of the 2008 event, discusses the mechanisms for the Wenchuan quake itself and the implications for our understanding of the eastern margin of the Tibetan Plateau, the ongoing risk from quake-induced landslides, and the societal impacts of the earthquake (Introduction) |
| Note de contenu : |
Bibliogr. Ã la fin des articles
Articles : Resilience from ruin - Beware of slowly slipping faults - The landslide story - Bottom-up disaster resilience - Topography reveals seismic hazard - Tectonics : Reanimating eastern Tibet - Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging - Mass wasting triggered by the 2008 Wenchuan earthquake is greater than orogenic growth - Two-phase growth of high topography in eastern Tibet during the Cenozoic - Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin - Uplift of the Longmen Shan and Tibetan plateau, and the 2008 Wenchuan (M = 7.9) earthquake .-Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake - Rupture of deep faults in the 2008 Wenchuan earthquake and uplift of the Longmen Shan |
5 Years after the Wenchuan Earthquake [texte imprimé] . - London : Nature Publishing Group, 2013 . - 1 vol. (52 p.) : ill., graph., fig., tabl. ; 28 cm. - ( Nature Collections) . PPN 280354738
Compilation d'articles parus dans Nature Geoscience Langues : Anglais ( eng)
| Tags : |
Séisme de Wenchuan (2008) Wenchuan Earthquake, China, 2008 |
| Index. décimale : |
551.220 951 Tremblements de terre - Chine et territoires adjacents (Tibet, Sinkiang, Mongolie, Mandchourie) |
| Résumé : |
The Wenchuan earthquake that occurred in southwest China on 12 May 2008 killed more than 80,000 people and displaced millions. Five years on, many of the affected communities have made a good recovery – at least until the most recent quake in April 2013 wreaked further havoc in the region. The devastating 2008 event has helped invigorate research into earthquake hazards. A collection of opinion pieces, published in Nature Geoscienceto mark the fifth anniversary of the 2008 event, discusses the mechanisms for the Wenchuan quake itself and the implications for our understanding of the eastern margin of the Tibetan Plateau, the ongoing risk from quake-induced landslides, and the societal impacts of the earthquake (Introduction) |
| Note de contenu : |
Bibliogr. Ã la fin des articles
Articles : Resilience from ruin - Beware of slowly slipping faults - The landslide story - Bottom-up disaster resilience - Topography reveals seismic hazard - Tectonics : Reanimating eastern Tibet - Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging - Mass wasting triggered by the 2008 Wenchuan earthquake is greater than orogenic growth - Two-phase growth of high topography in eastern Tibet during the Cenozoic - Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin - Uplift of the Longmen Shan and Tibetan plateau, and the 2008 Wenchuan (M = 7.9) earthquake .-Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake - Rupture of deep faults in the 2008 Wenchuan earthquake and uplift of the Longmen Shan |
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