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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. -
Rare Birds in Iran in the Late 1960S and 1970S
Podoces, 2008, 3(1/2): 1–30 Rare Birds in Iran in the Late 1960s and 1970s DEREK A. SCOTT Castletownbere Post Office, Castletownbere, Co. Cork, Ireland. Email: [email protected] Received 26 July 2008; accepted 14 September 2008 Abstract: The 12-year period from 1967 to 1978 was a period of intense ornithological activity in Iran. The Ornithology Unit in the Department of the Environment carried out numerous surveys throughout the country; several important international ornithological expeditions visited Iran and subsequently published their findings, and a number of resident and visiting bird-watchers kept detailed records of their observations and submitted these to the Ornithology Unit. These activities added greatly to our knowledge of the status and distribution of birds in Iran, and produced many records of birds which had rarely if ever been recorded in Iran before. This paper gives details of all records known to the author of 92 species that were recorded as rarities in Iran during the 12-year period under review. These include 18 species that had not previously been recorded in Iran, a further 67 species that were recorded on fewer than 13 occasions, and seven slightly commoner species for which there were very few records prior to 1967. All records of four distinctive subspecies are also included. The 29 species that were known from Iran prior to 1967 but not recorded during the period under review are listed in an Appendix. Keywords: Rare birds, rarities, 1970s, status, distribution, Iran. INTRODUCTION Eftekhar, E. Kahrom and J. Mansoori, several of whom quickly became keen ornithologists. -
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 -
Rationale of the Study
European Online Journal of Natural and Social Sciences 2014; www.european-science.com Vol.3, No.4 Special Issue on Architecture, Urbanism, and Civil Engineering ISSN 1805-3602 Seeking Archetype of Water Storages of Qeshm Island Mehdi Bavaghar Zaeimi, Fatemeh Jafari* Young Researchers and Elite Club, Bandar Abbas branch, Islamic Azad University, Bandar Abbas, Iran *Email: [email protected] Abstract Throughout history, water as one of the most important natural factors played an important role in human life. In dry and waterless areas, people have always been in difficulty to provide and maintain and distribute water, and over centuries, different strategies have been applied to use water. In this article, water storage as one of the principle strategies to use water which has cultural and social indicators and dimensions was studied. Water storage as an urban structure remained from the past, is a valuable experience of Iranian art and belief values that can be used as a cultural and natural capital. Persian Gulf Islands, because of the lack of water has numerous water storages with different architecture plans and water storage can be called as a sign of this province beside wind towers. Wind towers is a phenomenon derived from confirmation of cultural and technical characteristics of humans with the natural features of the surrounding environment. With regard to drinking groundwater tables, Qeshm Island is one of the most disadvantaged areas of the country and people could already solve some of the problems related to annual lack of water by using their natural aptitudes in building water storage and well. -
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. -
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جامعة السلطان قابوس Sultan Qaboos University مجلة اﻵداب والعلوم اﻻجتماعية Journal of Arts & Social Sciences Description of Number, Person and Tense Features in the Verbal Morphologies of Jibbāli and Lari Khalsa Al Aghbari Muhammad Ourang Assistant Professor PhD candidate Department of English Language University of New South Wales and Literature, College of Arts and Social Sydney, Australia Sciences, Sultan Qaboos University [email protected] [email protected] Date received: 6/11/2015 Date of acceptance: : 28/06/2016 5 Description of Number, Person and Tense Features... Description of Number, Person and Tense Features in the Verbal Morphologies of Jibbāli and Lari Khalsa Al Aghbari and Muhammad Ourang Abstract: The study describes a few linguistic features in the verbal morphologies of two understudied languages: Jibbāli and Lari. Jibbāli, a Modern South Arabian language spoken in the southern part of the Sultanate of Oman and Lari, an Indo-Iranian language spoken in Iran, are at risk of being endangered due to the facts that (1) they lack a writing system, (2) they are not taught at schools, (3) they are not the official languages in Oman and Iran and, most importantly, (4) there is no effort recorded to preserve these languages. Therefore, the study aims at exposing the linguistic richness of Jibbāli and Lari through describing the tendencies of their verbal morphologies. This may help revitalize a substantial linguistic aspect of these languages. However, since this study is limited in space, it only focuses on certain morphological features which make these languages stand out. The researchers observe a few undocumented linguistic tendencies in Jibbāli and Lari which may attract attention for further studies. -
From the Persian Gulf and Oman Sea (Gobioidei: Gobiidae)
ArchiveIranian of Journal SID of Fisheries Sciences 19(2) 612-622 2020 DOI: 10.22092/ijfs.2018.119368. Shape variation of the Indian Ocean slender mudskipper, Scartelaos tenuis (Day, 1876) from the Persian Gulf and Oman Sea (Gobioidei: Gobiidae) Ghanbarifardi M.1*; Aliabadian M.2,3; Esmaeili H.R.4 Received: January 2017 Accepted: September 2017 Abstract The shape diversity among populations of Scartelaos tenuis (Day 1876) from five stations (194 specimens) in the Persian Gulf, Strait of Hormuz (Qeshm Island), and the Oman Sea were investigated. The shape variation was assessed by geometric morphometrics, using 14 morphological landmarks. The two sexes were not distinguishable by the shape. Fish samples were classified into two distinct groups, the fish from the Persian Gulf (Heleh and Asaluyeh), and the specimens of Qeshm Island and the Oman Sea (Chahoo, Dargahan and Jask). The Persian Gulf and the Oman Sea are characterized by specific environmental parameters of surface waters, including temperature and salinity. The shape discrepancies of Scartelaos tenuis specimens from different stations are probably because of ecological parameters of the Persian Gulf and Oman Sea. Our results suggest that the observed pattern of morphological variation is almost some kind of polyphenism induced by distinct environmental factors. Keywords: Geometric morphometrics, Environmental factors, Polyphenism, Scartelaos tenuis, Persian Gulf, Oman Sea Downloaded from jifro.ir at 8:41 +0430 on Saturday April 4th 2020 1-Department of Biology, Faculty of Sciences, University of Sistan and Baluchestan, Zahedan, Iran 2-Department of Biology, Faculty of Sciences, Ferdowsi University of Mashhad, Mashhad, Iran 3-Research Department of Zoological Innovations (RDZI), Institute of Applied Zoology, Faculty of Sciences, Ferdowsi University of Mashhad, Mashhad, Iran. -
Salt Plugs in the Eastern Zagros, Iran: Results of Regional Geological Reconnaissance
GeoLines (Praha), 7 (1998) 3 Salt Plugs in the Eastern Zagros, Iran: Results of Regional Geological Reconnaissance Pavel BOSÁK1, Josef JAROŠ2, Jiøí SPUDIL3, Petr SULOVSKÝ4 and Vladimír VÁCLAVEK5 1 Geological Institute, Czech Academy of Sciences, Rozvojová 135, 165 02 Praha 6, Czech Republic; e-mail: [email protected] 2 Institute of Geology and Paleontology, Faculty of Natural Sciences, Charles University, Albertov 6, 128 43 Praha 2, Czech Republic 3 GET Ltd., Korunovaèní 29, 170 00 Praha 7, Czech Republic, e-mail: [email protected] 4 Department of Mineralogy, Petrology and Geochemistry, Masaryk University, Kotláøská 2, 611 37 Brno, Czech Republic; e-mail: [email protected] 5 Pod Spoøilovem 2779, 141 00 Praha 4, Czech Republic ABSTRACT. Regional reconnaissance study of salt plugs cov- temperature is needed to start the glacier flow. Unbreached ered the area of about 50,000 square kilometers (coordinates salt plugs were discussed. Their occurrence is highly limited. It 53o50' to 56o30' E and 26o30' to 28o15‘N). Altogether 68 salt is shown, that “collapse structures” are connected rather with plugs were characterized from the viewpoint of their position other processes than solution collapse after leached salt. Tec- in the structure of area, morphological and evolution stages, tonic effects, erosion and pedimentation took part substantial- rock content and mineralization. ly in the formation of cauldrons. Linear cauldrons are connect- Prevailing amount of plugs lies in the flanks of anticline ed with tension regime in the apical zone of anticlines. Primary folds and is bounded to fold plunges and sigmoidal bends, where and secondary rim synclines have not been yet detected.