The Movement Potential Evaluation of the Active Faults Golbaf and Shahdad in Kerman Province
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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. -
Fxm2483part1index
UIT - BUREAU DES ITU - RADIOCOMMUNICATION UIT - OFICINA DE RADIOCOMMUNICATIONS BUREAU RADIOCOMUNICACIONES FXM provisoire / provisional N° 2483 Index / Indice Partie 1P / Part 1P / Parte 1P Date/Fecha: 26-11-2002 Détails des assignations de fréquence Particulars of frequency assignment Detalles de las notificaciones de asignación de reçues par le BR dans le format TerRaSys notices received by the BR in TerRaSys frecuencia recibidas por la BR en formato (voir CR/118). format (see CR/118). TerRaSys (ver CR/118). Cette partie 1P est aussi publiée en fichier This Part 1P is also published in Esta Parte 1P se publica también en el fichero MS-Access (mdb). Afin de faciliter l'utilisation MS-Access (mdb) file. In order to facilitate MS-Acces (mdb). Para facilitar la utilización del du fichier, le numéro d’index provisoire trouvé the use of the file, the provisional index mismo, el número de índice provisional que se en cette page d’index indique le numéro de number found in this index page indicates encuentra en esta página de índice indica el série de la notice dans le fichier. Veuillez the serial number of the notice in the file. número de serie de la notificación en dicho utiliser le programme fourni “FXM Part 1P Please use the supplied program “FXM Part fichero. Sírvase utilizar el programa suministrado: Software” pour visualiser les notices. 1P Software” to view the notices. “FXM Part 1P Software” para visualizar las notificaciones. Index Intent B 4B/5B 1A [MHz] 4A/5A 6A Adm. Ref. Identifier 248302543 ADD ARM ARM 890.200000 YEREVAN YE 03 -
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. -
BR IFIC N° 2509 Index/Indice
BR IFIC N° 2509 Index/Indice International Frequency Information Circular (Terrestrial Services) ITU - Radiocommunication Bureau Circular Internacional de Información sobre Frecuencias (Servicios Terrenales) UIT - Oficina de Radiocomunicaciones Circulaire Internationale d'Information sur les Fréquences (Services de Terre) UIT - Bureau des Radiocommunications Part 1 / Partie 1 / Parte 1 Date/Fecha: 16.12.2003 Description of Columns Description des colonnes Descripción de columnas No. Sequential number Numéro séquenciel Número sequencial BR Id. BR identification number Numéro d'identification du BR Número de identificación de la BR Adm Notifying Administration Administration notificatrice Administración notificante 1A [MHz] Assigned frequency [MHz] Fréquence assignée [MHz] Frecuencia asignada [MHz] Name of the location of Nom de l'emplacement de Nombre del emplazamiento de 4A/5A transmitting / receiving station la station d'émission / réception estación transmisora / receptora 4B/5B Geographical area Zone géographique Zona geográfica 4C/5C Geographical coordinates Coordonnées géographiques Coordenadas geográficas 6A Class of station Classe de station Clase de estación Purpose of the notification: Objet de la notification: Propósito de la notificación: Intent ADD-addition MOD-modify ADD-additioner MOD-modifier ADD-añadir MOD-modificar SUP-suppress W/D-withdraw SUP-supprimer W/D-retirer SUP-suprimir W/D-retirar No. BR Id Adm 1A [MHz] 4A/5A 4B/5B 4C/5C 6A Part Intent 1 103058326 BEL 1522.7500 GENT RC2 BEL 3E44'0" 51N2'18" FX 1 ADD 2 103058327 -
Kerman Province
In TheGod Name of Kerman Ganjali khan water reservoir / Contents: Subject page Kerman Province/11 Mount Hezar / 11 Mount joopar/11 Kerman city / 11 Ganjalikhan square / 11 Ganjalikhan bazaar/11 Ganjalikhan public bath /12 Ganjalikhan Mint house/12 Ganjalikhan School/12 Ganjalikhan Mosque /13 Ganjalikhan Cross market place /13 Alimardan Khan water reservoir /13 Ibrahimkhan complex/ 13 Ibrahimkhan Bazaar/14 Ibrahimkhan School /14 Ibrahimkhan bath/14 Vakil Complex/14 Vakil public bath / 14 Vakil Bazaar / 16 Vakil Caravansary / 16 Hajagha Ali complex / 16 Hajagha Ali mosque / 17 Hajagha Ali bazaar / 17 Hajagha Ali reservoir / 17 Bazaar Complex / 17 Arg- Square bazaar / 18 Kerman Throughout bazaar / 18 North Copper Smithing bazaar / 18 Arg bazaar / 18 West coppersmithing bazaar / 18 Ekhteyari bazaar / 18 Mozaffari bazaar / 19 Indian Caravansary / 19 Golshan house / 19 Mozaffari grand mosque / 19 Imam mosque / 20 Moshtaghieh / 20 Green Dome / 20 Jebalieh Dome / 21 Shah Namatollah threshold / 21 Khaje Etabak tomb / 23 Imam zadeh shahzadeh Hossien tomb / 23 Imam zadeh shahzadeh Mohammad / 23 Qaleh Dokhtar / 23 Kerman fire temple / 24 Moaidi Ice house / 24 Kerman national library / 25 Gholibig throne palace / 25 Fathabad Garden / 25 Shotor Galoo / 25 Shah zadeh garden / 26 Harandi garden / 26 Arg-e Rayen / 26 Ganjalikhan anthropology museum / 27 Coin museum / 27 Harandi museum garden / 27 Sanatti museum / 28 Zoroasterian museum / 28 Shahid Bahonar museum / 28 Holy defense museum / 28 Jebalieh museum / 29 Shah Namatollah dome museum / 29 Ghaem wooden -
Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト
Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト ● Asia 4 Bangladesh 7 China アジア バングラデシュ 中国 1 Afghanistan 9 Khulna 6 Hangzhou アフガニスタン クルナ 杭州（ハンチォウ） 1 Herat 10 Kotwalipara 7 Wuhan ヘラート コタリパラ 武漢（ウハン） 2 Kabul 11 Meherpur 8 Cyprus カブール メヘルプール キプロス 3 Nili 12 Moulvibazar 1 Aglantzia ニリ モウロビバザール アグランツィア 2 Armenia 13 Narayanganj 2 Ammochostos (Famagusta) アルメニア ナラヤンガンジ アモコストス（ファマグスタ） 1 Yerevan 14 Narsingdi 3 Kyrenia エレバン ナールシンジ キレニア 3 Azerbaijan 15 Noapara 4 Kythrea アゼルバイジャン ノアパラ キシレア 1 Agdam 16 Patuakhali 5 Morphou アグダム（県） パトゥアカリ モルフー 2 Fuzuli 17 Rajshahi 9 Georgia フュズリ（県） ラージシャヒ ジョージア 3 Gubadli 18 Rangpur 1 Kutaisi クバドリ（県） ラングプール クタイシ 4 Jabrail Region 19 Swarupkati 2 Tbilisi ジャブライル（県） サルプカティ トビリシ 5 Kalbajar 20 Sylhet 10 India カルバジャル（県） シルヘット インド 6 Khocali 21 Tangail 1 Ahmedabad ホジャリ（県） タンガイル アーメダバード 7 Khojavend 22 Tongi 2 Bhopal ホジャヴェンド（県） トンギ ボパール 8 Lachin 5 Bhutan 3 Chandernagore ラチン（県） ブータン チャンダルナゴール 9 Shusha Region 1 Thimphu 4 Chandigarh シュシャ（県） ティンプー チャンディーガル 10 Zangilan Region 6 Cambodia 5 Chennai ザンギラン（県） カンボジア チェンナイ 4 Bangladesh 1 Ba Phnom 6 Cochin バングラデシュ バプノム コーチ（コーチン） 1 Bera 2 Phnom Penh 7 Delhi ベラ プノンペン デリー 2 Chapai Nawabganj 3 Siem Reap Province 8 Imphal チャパイ・ナワブガンジ シェムリアップ州 インパール 3 Chittagong 7 China 9 Kolkata チッタゴン 中国 コルカタ 4 Comilla 1 Beijing 10 Lucknow コミラ 北京（ペイチン） ラクノウ 5 Cox's Bazar 2 Chengdu 11 Mallappuzhassery コックスバザール 成都（チォントゥ） マラパザーサリー 6 Dhaka 3 Chongqing 12 Meerut ダッカ 重慶（チョンチン） メーラト 7 Gazipur 4 Dalian 13 Mumbai (Bombay) ガジプール 大連（タァリィェン） ムンバイ（旧ボンベイ） 8 Gopalpur 5 Fuzhou 14 Nagpur ゴパルプール 福州（フゥチォウ） ナーグプル 1/108 Pages -
BR IFIC N° 2728 Index/Indice
BR IFIC N° 2728 Index/Indice International Frequency Information Circular (Terrestrial Services) ITU - Radiocommunication Bureau Circular Internacional de Información sobre Frecuencias (Servicios Terrenales) UIT - Oficina de Radiocomunicaciones Circulaire Internationale d'Information sur les Fréquences (Services de Terre) UIT - Bureau des Radiocommunications Part 1 / Partie 1 / Parte 1 Date/Fecha 18.09.2012 Description of Columns Description des colonnes Descripción de columnas No. Sequential number Numéro séquenciel Número sequencial BR Id. BR identification number Numéro d'identification du BR Número de identificación de la BR Adm Notifying Administration Administration notificatrice Administración notificante 1A [MHz] Assigned frequency [MHz] Fréquence assignée [MHz] Frecuencia asignada [MHz] Name of the location of Nom de l'emplacement de Nombre del emplazamiento de 4A/5A transmitting / receiving station la station d'émission / réception estación transmisora / receptora 4B/5B Geographical area Zone géographique Zona geográfica 4C/5C Geographical coordinates Coordonnées géographiques Coordenadas geográficas 6A Class of station Classe de station Clase de estación Purpose of the notification: Objet de la notification: Propósito de la notificación: Intent ADD-addition MOD-modify ADD-ajouter MOD-modifier ADD-añadir MOD-modificar SUP-suppress W/D-withdraw SUP-supprimer W/D-retirer SUP-suprimir W/D-retirar No. BR Id Adm 1A [MHz] 4A/5A 4B/5B 4C/5C 6A Part Intent 1 112143773 ARG 7135.0000 COLONIA AURORA ARG 54W30'53'' 27S28'19'' FX 1 ADD 2 -
Southeastern Iran Is Frontier Territory
©Lonely Planet Publications Pty Ltd S o u t h e a s t e r n I r a n ﺍﻳﺮﺍﻥ ﺟﻨﻮﺏ ﺷﺮﻗﯽ Why Go? Meymand......................222 Southeastern Iran is frontier territory. It combines harsh Kerman .........................222 landscapes, periodic banditry and warm welcomes to form Around Kerman ............229 a unique and exotic travelling experience. There are some Rayen .............................231 dangers; see the box, p 233 , before heading this way. The re- gion stretches east across ancient Kerman province, through Bam ...............................231 high deserts scarred by brown snow-capped mountain Zahedan .......................233 ranges and coloured by occasional oasis towns and seasonal Mirjaveh ........................235 lakes. Kerman, the main city, is, in eff ect, the cultural bor- der separating the Persians and the more eastern-oriented Baluchis, whose dress and customs feel more Pakistani. Best Places to Eat Following old caravan routes southeast across the edge of the forbidding Dasht-e Lut, most travellers will stop in » Restaurant Ganjali Khan historic Bam and, if heading to Pakistan, in Zahedan, where (p 228 ) smugglers criss-cross the deserts and the rule of law is ten- » Akhavan Hotel Restaurant uous. Kerman city is the launch pad for the surrounding (p 228 ) historic towns and incredible desert landscapes, including » Hamam-e Vakil Chay- Mahan and the Kaluts. khaneh (p 228 ) » Bagh-e Khannevadeh (p 233 ) When to Go » Ghana-at Faludeh (p 228 ) Much of southeastern Iran is desert or semidesert and the best time to avoid the heat is between around November Best Places to and March. During these times daytime temperatures are Stay often quite comfortable between about 10°C and 20°C, but overnight temperatures regularly fall to -10°C. -
Bam Earthquake, Iran 26 December 2003 1
THE BAM, IRAN EARTHQUAKE OF 26 DECEMBER 2003 Field Investigation Report Prepared By: Dr. Ali Reza Manafpour, Halcrow Group Limited Acknowledgements: The author gratefully acknowledges the financial support of Halcrow Group Limited for this earthquake field investigation. Also the following individuals and organizations are acknowledged for their kind support, assistance and information in preparing this report. Dr. Stewart Gallocher, Mr. Angus McConnell and Mr. Colin Robertson of the Energy and Special Structure’s Group within Halcrow Group Limited, for their encouragement, kind advice and comments as well as facilitating the field visit. The Institution of Structural Engineers’ Earthquake Engineering Field Investigation Team (EEFIT) for their continuous support and interest in publishing the report. Mr. Tony Morrison from Halcrow Group and staff at the Acasia International’s Tehran office for their local arrangements in Tehran. Dr. Farzad Naeim EERI’s Learning From Earthquake’s team leader to Bam for his generous cooperation allowing the author to join their team briefing in IIEES. Professor Ghafori-Ashtiani president of IIEES, Iran, and his colleagues for providing an excellent briefing of various aspects of the earthquake. Mr. Alireza Mostafa-Neghad director general of the Ministry of Housing and Urban Development’s (MUHD) provincial office in Kerman for his kind reception and facilitation of travelling and accommodation in Bam. Mr. Mahmood Iranmanesh, head of the Technical Division in MHUD’s provincial office in Kerman for his local and professional information during the visit and providing his own photos and video film. Dr. Ali Ebrahimi from Kerman University who generously offered his time and assistance for local arrangements in Kerman. -
Geomorphic Systems Affecting the Kerman
University College of Takestan Available online at http://UCTjournals.com UCT Journal of Social Sciences and Humanities Research UCT . J. Soc. Scien. Human. Resear.(UJSSHR) Volume 1,Issue 1 06 - 11 (2013) ISSN:2382-9753 X Geomorphic systems affecting the Kerman Hossein Ghazanfarpour¹, Mohsen Pourkhosravani²*, S. Elham Mousavi³ ¹Assistant Professor, Department Of Geography, Shahid Bahonar University , Kerman, Iran ²Assistant Professor, Department Of Geography, Shahid Bahonar University, Kerman, Iran ³M.S. Student In Geography And Urban Planning, Payame Noor University, Ahvaz, Iran *Corresponding author, Email: [email protected] ABSTRACT Original Article: According to geomorphic systems affecting the settlement of areas, including in the planning and urban management. Due to the geographical location and structural the Kerman and performance of various systems of agents, such systems are alluvial, Aeolian and morphotectonic Implementation and management of all development Received 10 Nov. 2013 plans need to be obsessively this space very carefully done. The incidence of serious risks such as ground Accepted 23 Dec. 2013 subsidence, loss of water resources, tectonic activity and Aeolian processes in the atmosphere is solid evidence of this claim. Kerman is located at a point that many factors can affect its normal study of factors influencing the Published 30 Dec. 2013 reduction of environmental hazards can be effective. The purpose of this study demonstrates the effect of natural factors and the impact of Kerman urban development on the intensity of negative factors affecting external. This research is trying to use GIS techniques to evaluate geomorphic systems the Kerman range of factors influencing the mapping of processes to check. -
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Model Paper from 4Icsz [Text]
THE CO-SEISMIC COULOMB STRESS CHANGES IN THE SOUTHEAST AND NORTHWEST OF IRANIAN PLATEAU Behnam MALEKI ASAYESH1, Hamid ZAFARANI2, Majid MAHOOD3, Saeed ZAREI4 ABSTRACT Iranian Plateau has been frequently struck by catastrophic earthquakes resulting in the massive loss of life, large masses homeless and disrupting their agricultural and industrial lifelines. Southeast of Iran experienced 8 earthquakes during 30 years from 1981 to 2011. Northwest of Iran experienced historical and instrumental large earthquakes too. On 11 August 2012, a strong earthquake with magnitude Mw 6.4 occurred in Ahar- Varzaghan region, NW of Iran. It followed by another strong earthquake with magnitude Mw 6.2 after 11 minutes. The influence of static stress transfer due to moderate-to-large earthquakes on the occurrence of future earthquakes had been proved by numerous studies. This effect in triggering future events and spatial distribution of aftershocks can be explained by using the Coulomb stress changes theory. We calculated the static Coulomb stress changes for the southeast of Iran due to earthquake sequence from 1981 and for the northwest of Iran due to Ahar-Varzaghan earthquakes. In the southeast of Iran, our calculations showed a positive stress changes due to previous events on the rupture plane of next earthquake and only plane of the Rigan earthquake of 2010 December 20 received negative stress changes. Also, we calculated imparted stress changes on the surrounding active faults and showed that hypocenter of recent Hojedk earthquakes (2017 December 1 and 12) with a moment magnitude of 6.1, 6.2, and 6.1 respectively, received positive stress changes. -
Islamic Republic of Iran As Affected Country Party
United Nations Convention to Combat Desertification Performance Review and Assessment of Implementation System Fifth reporting cycle, 2014-2015 leg Report from Islamic Republic of Iran as affected country Party July 25, 2014 Contents I. Performance indicators A. Operational objective 1: Advocacy, awareness raising and education Indicator CONS-O-1 Indicator CONS-O-3 Indicator CONS-O-4 B. Operational objective 2: Policy framework Indicator CONS-O-5 Indicator CONS-O-7 C. Operational objective 3: Science, technology and knowledge Indicator CONS-O-8 Indicator CONS-O-10 D. Operational objective 4: Capacity-building Indicator CONS-O-13 E. Operational objective 5: Financing and technology transfer Indicator CONS-O-14 Indicator CONS-O-16 Indicator CONS-O-18 II. Financial flows Unified Financial Annex III. Additional information IV. Submission Islamic Republic of Iran 2/225 Performance indicators Operational objective 1: Advocacy, awareness raising and education Number and size of information events organized on the subject of desertification, land degradation CONS-O-1 and drought (DLDD) and/or DLDD synergies with climate change and biodiversity, and audience reached by media addressing DLDD and DLDD synergies Percentage of population informed about DLDD and/or DLDD synergies 30 % 2018 Global target with climate change and biodiversity National contribution Percentage of national population informed about DLDD and/or DLDD 2011 to the global target synergies with climate change and biodiversity 27 2013 2015 2017 2019 % Year Voluntary national Percentage