✦ LIBER ✦

The Murdjadjo, Western Algeria, fault-related fold: Implications for seismic hazard

✍ Scribed by Youcef Bouhadad

Book ID: 110308766
Publisher: Springer
Year: 2001
Tongue: English
Weight: 1012 KB
Volume: 5
Category: Article
ISSN: 1383-4649
DOI: 10.1023/a:1012039900248

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Significant Earthquakes on the Enriquill

Significant Earthquakes on the Enriquillo Fault System, Hispaniola, 1500-2010: Implications for Seismic Hazard

✍ Bakun, William H. (author);Flores, Claudia H. (author);ten Brink, Uri S. (author 📂 Article 📅 2012 🏛 Seismological Society of America 🌐 English ⚖ 714 KB

Significant Earthquakes on the Enriquill

Significant Earthquakes on the Enriquillo Fault System, Hispaniola, 1500-2010: Implications for Seismic Hazard

✍ Bakun, William H. (author);Flores, Claudia H. (author);ten Brink, Uri S. (author 📂 Article 📅 2012 🏛 Seismological Society of America 🌐 English ⚖ 714 KB

Advances in active faulting studies and

Advances in active faulting studies and their implications for seismic hazard assessment in the Euro-Mediterranean region

✍ Gianluca Valensise; Duvvet Atakan 📂 Article 📅 2004 🏛 Springer 🌐 English ⚖ 415 KB

Seismic behaviour of the North Anatolian

Seismic behaviour of the North Anatolian Fault beneath the Sea of Marmara (NW Turkey): implications for earthquake recurrence times and future seismic hazard

✍ Murat Utkucu; Zakir Kanbur; Ömer Alptekin; Fatih Sünbül 📂 Article 📅 2008 🏛 Springer Netherlands 🌐 English ⚖ 744 KB

Evidence for fault-related directionalit

Evidence for fault-related directionality and localized site effects from strong motion recordings of the 2003 Boumerdes (Algeria) earthquake: Consequences on damage distribution and the Algerian seismic code

✍ Nasser Laouami; Abdennasser Slimani; Youcef Bouhadad; Jean-Luc Chatelain; Ali No 📂 Article 📅 2006 🏛 Elsevier Science 🌐 English ⚖ 919 KB

The Algiers-Boumerdes region has been struck by a destructive magnitude 6.8 (M w ) earthquake on May 21, 2003. The study presented in this paper is based on main shock strong motions from 13 stations of the Algerian accelerograph network. A maximum 0.58g peak ground acceleration (PGA) has been recor