Surface Rupture Database for Seismic Hazard Assessment
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Bam, Iran Earthquake of 26 December 2003, Mw6.5: a Study on the Strong Ground Motions
13th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 8001 BAM, IRAN EARTHQUAKE OF 26 DECEMBER 2003, MW6.5: A STUDY ON THE STRONG GROUND MOTIONS Mehdi ZARE1 SUMMARY The Bam earthquake of 26 December 2003 (Mw6.5) occurred at 01:56:56 (GMT, 05:26:56 local time) around the city of Bam in the southeast of Iran. The Bam earthquake of 26/12/2003 (Mw6.5) has demolished the city of Bam, having a population of about 100000 at the time of the earthquake. The Bam fault - which was mapped before the event on the geological maps - has been reactivated during the 26/12/2003 earthquake. It seems that a length of about 10km (at the surface) of this fault has been reactivated, where it passed exactly from the east of the city of Bam. The fault has a slop towards the west and the foci of the event was located closed to the residential area (almost beneath the city of Bam). This caused a great damage in the macroseismic epicentral zone; however the strong motions have been attenuated very rapidly, specially towards the east-and west (fault normal) direction. The vertical directivity effects caused the amplification of the low frequency motions in the fault-normal direction as well as the greater amplitude of the motion on the vertical direction. INTRODUCTION The Bam earthquake of 26/12/2003 (Mw6.5) demolished the city of Bam in the southeast of Iran (Figure- 1). The earthquake happened at 5:26 am local time when most of the inhabitants were slept, that can be one of the causes of the great life losses. -
Introduction San Andreas Fault: an Overview
Introduction This volume is a general geology field guide to the San Andreas Fault in the San Francisco Bay Area. The first section provides a brief overview of the San Andreas Fault in context to regional California geology, the Bay Area, and earthquake history with emphasis of the section of the fault that ruptured in the Great San Francisco Earthquake of 1906. This first section also contains information useful for discussion and making field observations associated with fault- related landforms, landslides and mass-wasting features, and the plant ecology in the study region. The second section contains field trips and recommended hikes on public lands in the Santa Cruz Mountains, along the San Mateo Coast, and at Point Reyes National Seashore. These trips provide access to the San Andreas Fault and associated faults, and to significant rock exposures and landforms in the vicinity. Note that more stops are provided in each of the sections than might be possible to visit in a day. The extra material is intended to provide optional choices to visit in a region with a wealth of natural resources, and to support discussions and provide information about additional field exploration in the Santa Cruz Mountains region. An early version of the guidebook was used in conjunction with the Pacific SEPM 2004 Fall Field Trip. Selected references provide a more technical and exhaustive overview of the fault system and geology in this field area; for instance, see USGS Professional Paper 1550-E (Wells, 2004). San Andreas Fault: An Overview The catastrophe caused by the 1906 earthquake in the San Francisco region started the study of earthquakes and California geology in earnest. -
Data Collection Survey Report on Earthquake Management in Iran
DATA COLLECTION SURVEY REPORT ON EARTHQUAKE MANAGEMENT IN IRAN AUGUST 2019 JAPAN INTERNATIONAL COOPERATION AGENCY (JICA) JAPAN METEOROLOGICAL BUSINESS SUPPORT CENTER AND YACHIYO ENGINEERING CO., LTD. 7R JR 19-010 Summary 1. Overview of Iran The Islamic Republic of Iran is located in the southwest Asia and the country has a mountainous area and a desert. The land area is around 1.6 million km2 and it is approx. 4.4 times1 that of Japan. It is bordered by the Caspian Sea, Turkmenistan, Azerbaijan and Armenia to the north, by Afghanistan and Pakistan to the east, by Turkey and Iraq to the west, and by the Persian Gulf, Oman, UAE, Qatar, Bahrain, Kuwait and Saudi Arabia to the south. The Zagros mountains, which run from the Iraqi border to the Persian Gulf coast, was formed as a result of a collision between the Arabian Plate and the Eurasian Plate. The Arabian Plate is still moving at a rate of around 25 mm a year, and the accumulation of seismic energy caused by its collision with the i Eurasian plate produces frequent earthquakes in Iran. The capital, Tehran, experiences major earthquakes with an approximate 150-year cycle. Accordingly, there is a high interest in reducing earthquake risk. 2. Background and Outline of the Project Accordingly, the national government has laid out policies for goals such as enhancement of measures against natural disasters and strengthened research for earthquake risk mitigation through the expansion of earthquake observation networks in its laws and development plans. Against this background, seismic activity is monitored extensively on a nationwide basis, and earthquake-related research is actively carried out. -
Western States Seismic Policy Council Policy Recommendation 18-3
WESTERN STATES SEISMIC POLICY COUNCIL POLICY RECOMMENDATION 18-3 Definitions of Recency of Surface Faulting for the Basin and Range Province Policy Recommendation 18-3 WSSPC recommends that each state in the Basin and Range physiographic province (BRP), through consultation with state and federal geological surveys and other earthquake-hazard experts, define scientifically and societally relevant categories for recency of surface faulting (generally earthquake magnitude ≥M 6.5). WSSPC further recommends that in the absence of information to the contrary, all Quaternary faults be considered to have the recency of activity documented in the USGS Quaternary fault and fold database until more adequate data can be developed. Executive Summary Fault recency definitions are limited to the Quaternary because this period of geologic time is considered by the scientific community to be most relevant to paleoseismic studies of earthquake faults (Machette and others, 2004). The recency class of a fault is the youngest class based on the demonstrated age of most recent surface faulting. Latest Pleistocene-Holocene faults are included within the definition of late Quaternary faults, and both latest Pleistocene-Holocene and late Quaternary faults are included in Quaternary faults. Establishment/definition of surface-faulting recency categories are based on the ways that faults are portrayed on geologic maps and on the availability of geologic data in the BRP. Policy makers (owners, regulators, governmental agencies) should consult with state and federal geological surveys and other earthquake-hazard experts in using these recency categories and additional geologic data in developing definitions of hazardous faults to be considered in planning for development or infrastructure projects. -
Insights Into the Aftershocks and Inter-Seismicity for Some Large Persian Earthquakes
Journal of Sciences, Islamic Republic of Iran 26(1): 35 - 48 (2015) http://jsciences.ut.ac.ir University of Tehran, ISSN 1016-1104 Insights into the Aftershocks and Inter-Seismicity for Some Large Persian Earthquakes M. Nemati* Department of Geology, Faculty of Science, Shahid Bahonar University of Kerman, Kerman City, Islamic Republic of Iran Earthquake Research Center, Shahid Bahonar University of Kerman, Kerman City, Islamic Republic of Iran Received: 8 July 2014 / Revised: 23 September 2014 / Accepted: 14 December 2014 Abstract This paper focuses on aftershocks behavior and seismicity along some co-seismic faults for large earthquakes in Iran. The data of aftershocks and seismicity roughly extracted from both the Institute of Geophysics the University of Tehran (IGUT) and International Seismological Center (ISC) catalogs. Apply some essential methods on 43 large earthquakes data; like the depth, magnitude as well as the aftershock data; resulted knowledge about some relations between earthquake characteristics. We found ~16.5km for deep seated co-seismic fault length for the 2005 Dahouieh Zarand earthquake (MW 6.4) considering the dimension of the main cluster of aftershocks. Moreover, a slightly decrease in aftershocks activity was observed with increase in depth of the mainshocks for some Iranian earthquakes. Also the clustered aftershocks for the 1997 Zirkuh-e Qaen earthquake (MW 7.1) showed a clear decrease in maximum magnitude of the aftershocks per day elapsed from mainshock. Finally, we could explore an anti-correlation between aftershocks distribution and post microseismicity along co-seismic faults for both Dahouieh and Qaen earthquakes. Keywords: Aftershock; Mainshock; Magnitude; Seismicity and Persia. mainshock hypocenter immediately after the Introduction earthquake occurrence. -
Late Quaternary Faulting in the Kaikoura Region, Southeastern Marlborough, New Zealand
AN ABSTRACT OF THE THESIS OF Russell J. Van Dissen for the degree of Master of Science in Geology presented on February 15, 1989. Title: Late Quaternary Faulting in the Kaikoura Region, Southeastern Marlborough, New Zealand Redacted for privacy Abstract approved: Dr. Robert 8.0eats Active faults in the Kaikoura region include the Hope, Kekerengu, and Fidget Faults, and the newly discovered Jordan Thrust, Fyffe, and Kowhai Faults. Ages of faulted alluvial terraces along the Hope Fault and the Jordan Thrust were estimated using radiocarbon-calibrated weathering-rind measurements on graywacke clasts. Within the study area, the Hope Fault is divided, from west to east, into the Kahutara, Mt. Fyffe, and Seaward segments. The Kahutara segment has a relatively constant Holocene right-lateral slip rate of 20-32 mm/yr, and an earthquake recurrence interval of 86 to 600 yrs: based on single-event displacements of 3 to 12 m. The western portion of the Mt. Fyffe segment has a minimum Holocene lateral slip rate of 16 + 5 mm/yr .(southeast side up); the eastern portion has horizontal and vertical slip rates of 4.8+ 2.7 mm/yr and 1.7 + 0.2 mm/yr, respectively (northwest side up). There is no dated evidence for late Quaternary movementon the Seaward segment, and its topographic expression is much more subdued than that of the two western segments. The Jordan Thrust extends northeast from the Hope Fault, west of the Seaward segment. The thrust has horizontal and vertical slip rates of 2.2 + 1.3 mm/yr and 2.1 + 0.5 mm/yr, respectively (northwest side up), and a maximum recurrence interval of 1200 yrs: based on 3 events within the last 3.5 ka. -
Active and Potentially Active Faults in Or Near the Alaska Highway Corridor, Dot Lake to Tetlin Junction, Alaska
Division of Geological & Geophysical Surveys PRELIMINARY INTERPRETIVE REPORT 2010-1 ACTIVE AND POTENTIALLY ACTIVE FAULTS IN OR NEAR THE ALASKA HIGHWAY CORRIDOR, DOT LAKE TO TETLIN JUNCTION, ALASKA by Gary A. Carver, Sean P. Bemis, Diana N. Solie, Sammy R. Castonguay, and Kyle E. Obermiller September 2010 THIS REPORT HAS NOT BEEN REVIEWED FOR TECHNICAL CONTENT (EXCEPT AS NOTED IN TEXT) OR FOR CONFORMITY TO THE EDITORIAL STANDARDS OF DGGS. Released by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys 3354 College Rd. Fairbanks, Alaska 99709-3707 $4.00 CONTENTS Abstract ............................................................................................................................................................ 1 Introduction ....................................................................................................................................................... 1 Seismotectonic setting of the Tanana River valley region of Alaska ................................................................ 3 2008 fi eld studies .............................................................................................................................................. 5 Field and analytical methods ............................................................................................................................ 5 Dot “T” Johnson fault ....................................................................................................................................... 7 Robertson -
Major Earthquakes of the Past Decade
Trauma Mon.2012;17(1):219-229. DOI: 10.5812/traumamon.4519 KOWSAR Major Earthquakes of the Past Decade (2000-2010): A Comparative Review of Various Aspects of Management Mohammad Hosein Kalantar Motamedi 1 *, Masoud Sagafinia 1, Ali Ebrahimi 1, Ehsan Shams 1, Mostafa Kalantar Motamedi 1 1 Trauma Research Center, Baqiyatallah University of Medical Sciences, Tehran, IR Iran ARTICLE INFO ABSTRACT Article type: Objectives: This article sought to review and compare data of major earthquakes of the past Review Article decade and their aftermath in order to compare the magnitude, death toll, type of injuries, management procedures, extent of destruction and effectiveness of relief efforts. Article history: Materials and Methods: A retrospective study of the various aspects of management and Received: 16 Feb 2012 aftermath of 5 major earthquakes of the past decade (2000–2010) was undertaken. This in- Revised: 02 Mar 2012 cluded earthquakes occurring in Bam Iran, Sichuan China, Port-au-Prince Haiti, Kashmir Pak- Accepted: 03 Mar 2012 istan and Ica Peru. A literature search was done via computer of published articles (indexed in Pubmed). The issues assessed included: 1)Local magnitude,2)Type of building structure Keywords: 3)Time of the earthquake (day/time/season), 4)Time to rescue, 5)Triage, Transfer, and Treat- Earthquakes ment 6) Distribution of casualties (dead/ injured), 7)Degree of city damage, 8)Degree of dam- Review age to health facilities, 9)Field hospital availability, 10)International aid, 11)Air transfer, 12) Disasters Telecommunication systems availability, 13) PTSD prevalence, 14) Most common injury and Risk Management 15) Most common disease outbreak. -
Bam Earthquake, Iran: Lessons on the Seismic Behaviour of Building Structures
th The 14 World Conference on Earthquake Engineering October 12-17, 2008, Beijing, China BAM EARTHQUAKE, IRAN: LESSONS ON THE SEISMIC BEHAVIOUR OF BUILDING STRUCTURES 1 A. R. Manafpour 1 Structural Engineer, Halcrow Group Limited , Power and Structures, Glasgow, UK ABSTRACT : The Bam earthquake on 26 December 2003 with magnitude Mw=6.6 destroyed most of the city of Bam in Iran and nearby villages, and killed more than 26,000 people. The earthquake was by far the most devastating earthquake in the history of the region around Bam. After the earthquake the author undertook a field investigation and visited the affected area. The paper studies the structural damage on traditional as well as modern building structures during the earthquake. Adobe, masonry, steel and reinforced concrete structures are considered with some examples demonstrating the response of each type of the buildings. Discussion of the structural behavior is given with reference to existing seismic design codes and construction practice within the region. It is concluded that as a considerable number of buildings in central and eastern provinces of Iran, more specifically in villages, are built of mud-bricks and will not resist similar magnitude earthquakes. Due to specific materials and construction forms special strengthening procedures needs to be developed. KEYWORDS: Bam Earthquake, Adobe Structures, Earthquake Effects, Earthquake Filed Investigation, Seismic 1. INTRODUCTION A large earthquake with a magnitude of Mw=6.6 (USGS[3]) struck the city of Bam, located approximately 1000km southeast of Tehran, at 05:26:56 local time (01:56:56 GMT) on Friday 26th December 2003. The earthquake destroyed most of Bam city and the nearby villages and the official death toll exceeded 26,000 with more than 30,000 injuries and 75,000 left homeless. -
Fatemeh Farnaz Arefian Housing Reconstruction After the Bam
The Urban Book Series Fatemeh Farnaz Arefian Organising Post-Disaster Reconstruction Processes Housing Reconstruction after the Bam Earthquake The Urban Book Series Series Advisory Editors Fatemeh Farnaz Arefian, University College London, London, UK Michael Batty, University College London, London, UK Simin Davoudi, Newcastle University, Newcastle, UK Geoffrey DeVerteuil, Cardiff University, Cardiff, UK Karl Kropf, Oxford Brookes University, Oxford, UK Marco Maretto, University of Parma, Parma, Italy Vítor Oliveira, Porto University, Porto, Portugal Christopher Silver, University of Florida, Gainesville, USA Giuseppe Strappa, Sapienza University of Rome, Rome, Italy Igor Vojnovic, Michigan State University, East Lansing, USA Jeremy Whitehand, University of Birmingham, Birmingham, UK Aims and Scope The Urban Book Series is a resource for urban studies and geography research worldwide. It provides a unique and innovative resource for the latest developments in the field, nurturing a comprehensive and encompassing publication venue for urban studies, urban geography, planning and regional development. The series publishes peer-reviewed volumes related to urbanization, sustainabil- ity, urban environments, sustainable urbanism, governance, globalization, urban and sustainable development, spatial and area studies, urban management, urban infrastructure, urban dynamics, green cities and urban landscapes. It also invites research which documents urbanization processes and urban dynamics on a national, regional and local level, welcoming case -
Household Recovery and Housing Reconstruction After the 2003 Bam Earthquake in Iran
Université de Montréal HOUSEHOLD RECOVERY AND HOUSING RECONSTRUCTION AFTER THE 2003 BAM EARTHQUAKE IN IRAN by Mahmood Fayazi Faculté de l’aménagement A thesis presented to the Université de Montréal in fulfillment of the thesis requirement for the degree of Doctor of Philosophy in Built Environment Planning Montréal, Québec, Canada, 2017 © Mahmood Fayazi, 2017 Université de Montréal Université de Montréal Faculté des études supérieures Cette thèse intitulée : HOUSEHOLD RECOVERY AND HOUSING RECONSTRUCTION AFTER THE 2003 BAM EARTHQUAKE IN IRAN Présenté par : Mahmood Fayazi A été évaluée par un jury composé des personnes suivantes : - Mithra Zahedi (Présidente) ------------------------------------ - Gonzalo Lizarralde (Directeur) --------------------------------- - Christina Cameron (Member du jury) ------------------------ - Ipek Türeli (Examinateur externe) ---------------------------- Dedicated to my wife; for all her patience and unwavering love RÉSUMÉ La reconstruction de logements après désastre est un processus complexe qui joue un rôle crucial dans le rétablissement des ménages affectés. Dans les dernières décennies, les chercheurs ont examiné les programmes de rétablissement des ménages (à travers les concepts de la résilience, de la vulnérabilité, et du développement durable), et ils ont essayé de déterminer les variables à l’origine de leur succès et ou de leur échec. Cependant, plusieurs lacunes subsistent, notamment à propos du degré inégal de rétablissement parmi les différentes catégories de ménages, des compromis sur les objectifs du rétablissement, et de la collaboration insuffisante parmi les différentes parties prenantes. Cette étude vise à expliquer pourquoi et comment les projets de reconstruction ne réussissent pas à atteindre les objectifs de rétablissement. Elle cherche à révéler les principaux défis dans les initiatives visant à permettre aux ménages d’avoir un rétablissement équivalent et effectif durant les programmes de reconstruction. -
Surface Rupture of the 14 Nov 2016 Kaikoura
The 14 Nov 2016 Mw 7.8 Kaikoura Earthquake: Surface rupture ... and much more Pilar Villamor on behalf of the Earthquake Geology Response Team (54): Adrian Benson, Alan Bischoff, Alex Hatem, Andrea Barrier, Andy Nicol, Anekant Wandres, Biljana Lukovic, Brendan Hall, Caleb Gasston, Callum Margetts, Cam Asher, Chris Grimshaw, Chris Madugo, Clark Fenton, Dan Hale, David Barrell, David Heron, Delia Strong, Dougal Townsend, Duncan Noble, Jamie Howarth, Jarg Pettinga, Jesse Kearse, Jack Williams, Joel Bensing, John Manousakis, Josh Borella, Joshu Mountjoy, Julie Rowland, Kate Clark, Kate Pedley, Katrina Sauer, Kelvin Berryman, Mark Hemphill-Haley, Mark Stirling, Marlene Villeneuve, Matt Cockroft, Narges Khajavi, Nick Griffiths, Philip Barnes, Pilar Villamor, Rachel Carne, Robert Langridge, Robert Zinke, Russ van Dissen, Sam McColl, Simon Cox, Steve Lawson, Tim Little, Tim Stahl, Ursula Cochran, Virgina Toy, William Ries, Zoe Juniper GNS Science 14 November Kaikoura Earthquake This talk - Background - Kaikoura Earthquake - Seismicity, ground motions - InSAR and GNSS - Preliminary rupture models - Surface Rupture - Tsunami, Landslides (if we have time..) Photo: Sally Dellow, GNS Science Surface rupture of the Papatea Fault displacing the coastal platform, road, railway and hill country. GNS Science Background • The 14 Nov event occurred in the region between the Hikurangi subduction system of the North Island and the oblique collisional regime of the South Island (Alpine Fault) GNS Science Background • The 14 Nov event ruptured several faults that expand into different tectonic domains: o The strike-slip Marlborough fault system consists of a series of right lateral strike-slip faults, some with reverse component, that link to the Alpine fault on the west and to the subduction margin fore-arc to the east.