Geomorphic Systems Affecting the Kerman
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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. -
Review and Updated Checklist of Freshwater Fishes of Iran: Taxonomy, Distribution and Conservation Status
Iran. J. Ichthyol. (March 2017), 4(Suppl. 1): 1–114 Received: October 18, 2016 © 2017 Iranian Society of Ichthyology Accepted: February 30, 2017 P-ISSN: 2383-1561; E-ISSN: 2383-0964 doi: 10.7508/iji.2017 http://www.ijichthyol.org Review and updated checklist of freshwater fishes of Iran: Taxonomy, distribution and conservation status Hamid Reza ESMAEILI1*, Hamidreza MEHRABAN1, Keivan ABBASI2, Yazdan KEIVANY3, Brian W. COAD4 1Ichthyology and Molecular Systematics Research Laboratory, Zoology Section, Department of Biology, College of Sciences, Shiraz University, Shiraz, Iran 2Inland Waters Aquaculture Research Center. Iranian Fisheries Sciences Research Institute. Agricultural Research, Education and Extension Organization, Bandar Anzali, Iran 3Department of Natural Resources (Fisheries Division), Isfahan University of Technology, Isfahan 84156-83111, Iran 4Canadian Museum of Nature, Ottawa, Ontario, K1P 6P4 Canada *Email: [email protected] Abstract: This checklist aims to reviews and summarize the results of the systematic and zoogeographical research on the Iranian inland ichthyofauna that has been carried out for more than 200 years. Since the work of J.J. Heckel (1846-1849), the number of valid species has increased significantly and the systematic status of many of the species has changed, and reorganization and updating of the published information has become essential. Here we take the opportunity to provide a new and updated checklist of freshwater fishes of Iran based on literature and taxon occurrence data obtained from natural history and new fish collections. This article lists 288 species in 107 genera, 28 families, 22 orders and 3 classes reported from different Iranian basins. However, presence of 23 reported species in Iranian waters needs confirmation by specimens. -
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. -
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 -
Characteristics of 2017 Hojedk Earthquake Sequence in Kerman Province, Southeast Iran
Revista Geoaraguaia ISSN:2236-9716 Barra do Garças – MT v.10, n. esp. Geologia e Pedologia p.187-201. Dez-2020 CHARACTERISTICS OF 2017 HOJEDK EARTHQUAKE SEQUENCE IN KERMAN PROVINCE, SOUTHEAST IRAN CARACTERÍSTICAS DA SEQUÊNCIA DE TERREMOTO HOJEDK 2017 NA PROVÍNCIA DE KERMAN, SUDESTE DO IRÃ Nassim Mahdavi-Omran1 Mohammad-Reza Gheitanchi2 ABSTRACT Kerman province in southeast Iran, has experienced historical and instrumentally recorded earthquakes. In December 2017, three destructive earthquakes have occurred around Hojedk, in Kerman within 11 days. In this study, first the regional seismotectonics and seismicity is presented. Then, the source mechanisms of main shocks are modeled and the results are compared with the active faults and seismicity pattern is discussed. Moment tensor inversion in time domain is used to obtain the source mechanism of earthquakes. The results indicate that the mechanisms of main shocks and aftershocks are mainly reverse and are in agreement with the trend of tectonic forces as well as the mechanisms of other earthquakes. The epicentral distribution of aftershocks indicates two clusters. The spatial distributions of clusters are in agreement with the epicentral distribution of main shocks. The cluster around the first earthquake in EW cross section has a length 15-20 Km, while the cluster around the second and third has a length about 20-25 Km. The Hojedk earthquakes occurred along the northern extension of previous earthquakes where a kind of seismic gap could be observed and still exists. In 1972, within five days four earthquakes with magnitudes 5.5 to 6.2 occurred in Sefidabeh region in eastern edge of Lut block. -
Bonner Zoologische Beiträge
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Bonn zoological Bulletin - früher Bonner Zoologische Beiträge. Jahr/Year: 1978 Band/Volume: 29 Autor(en)/Author(s): Desfayes M., Praz J. C. Artikel/Article: Notes on Habitat and Distribution of Montane Birds in Southern Iran 18-37 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zoologicalbulletin.de; www.biologiezentrum.at Bonn. 18 zool. Beitr. Notes on Habitat and Distribution of Montane Birds in Southern Iran by M. DESFAYES, Washington, and J. C. PRAZ, Sempach This study was carried out in May and June 1975 to fill a gap in our knowledge of the breeding birds, their distribution and ecology, in the mountains of southern Iran. In these two months, most species occupy their breeding territories. Records from April or July are not always reliable as an indication of breeding, even if the bird is observed singing. While the avifauna of the northern parts of the country is relatively well-known, that of the southern highlands (above 2,000 meters) is poorly known. Blanford (1876) collected at Rayen (Rayun) 2100 m, and Hanaka, 2400 m, south-east of Kerman, just east of the Kuh-e Hazar, from 30 April to 2 May, and also at Khan-e Sorkh Pass 2550 m, 115 km south-west of Kerman on 23 May. Species collected in these areas by Blanford are: Columba palum- bus, Cuculus canorus, Melanocorypha bimaculata, Motacilla alba, Lanius collurio, Oenanthe picata, Oe. lugens, Oe. xanthoprymna, Montícola saxa- tilis, Sylvia curruca, Serinus pusillus, Acanthis cannabina, Emberiza bucha- nani, and E. -
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. -
Interseismic Slip-Rate of the Kuhbanan-Lakar Kuh Faults System: Using Insar Technique
EH-09260582 INTERSEISMIC SLIP-RATE OF THE KUHBANAN-LAKAR KUH FAULTS SYSTEM: USING INSAR TECHNIQUE Sajjad MOLAVI VARDANJANI M.Sc. Student, Graduate University of Advanced Technology, Kerman, Iran [email protected] Majid SHAHPASANDZADEH Associate Professor, Graduate University of Advanced Technology, Kerman, Iran [email protected] Ali ESMAEILY Assistant Professor, Dept. of Surveying Eng., Graduate University of Advanced Technology, Kerman, Iran [email protected] Mohammad Reza SEPAHVAND Assistant Professor, Graduate University of Advanced Technology, Kerman, Iran [email protected] Saeede KESHAVARZ Assistant Professor, Graduate University of Advanced Technology, Kerman, Iran [email protected] Keywords: Interseismic deformation, Geodetic fault slip-rate, InSAR, Kerman, Kuhbanan-Lakar Kuh fault system The Kuhbanan fault with ~ 300 km length, one of the largest seismogenic faults in the southeast of Iran, has caused st st several catastrophic earthquakes with Ms 5-6.2 in 20 -21 centuries (Table 1). Moreover, the corresponding cross-thrusts were also associated with at least five clusters of medium-magnitude earthquakes. The Lakar Kuh fault with ~160 km length run parallel to the Nayband fault (Figure 1). The slip-rate of faults and also the spatio-temporal distribution of large-magnitude shallow-depth earthquakes on the Kuhbanan-Lakar Kuh fault system, attain broad concern for seismic hazard assessment (Figure 1). The horizontal slip-rate of the Kuhbanan fault is estimated ~1–2 mm/yr (Walker et al., 2012). Furthermore, the total horizontal displacement of the fault is reported ~5–7 km, as determined by the offset geological markers (Table 2). Table 1. -
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 -
Coleoptera: Meloidae) in Kerman Province, Iran
J Insect Biodivers Syst 07(1): 1–13 ISSN: 2423-8112 JOURNAL OF INSECT BIODIVERSITY AND SYSTEMATICS Research Article https://jibs.modares.ac.ir http://zoobank.org/References/216741FF-63FB-4DF7-85EB-37F33B1182F2 List of species of blister beetles (Coleoptera: Meloidae) in Kerman province, Iran Sara Sadat Nezhad-Ghaderi1 , Jamasb Nozari1* , Arastoo Badoei Dalfard2 & Vahdi Hosseini Naveh1 1 Department of Plant Protection, Faculty of Agriculture and Natural Resources, University of Tehran, Karaj, Iran. [email protected]; [email protected]; [email protected] 2 Department of Biology, Faculty of Sciences, Shahid Bahonar University of Kerman, Kerman, Iran. [email protected] ABSTRACT. The family Meloidae Gyllenhaal, 1810 (Coleoptera), commonly known as blister beetles, exist in warm, dry, and vast habitats. This family was studied in Kerman province of Iran during 2018–2019. The specimens were Received: collected using sweeping net and via hand-catch. They were identified by the 23 December, 2019 morphological characters, genitalia, and acceptable identification keys. To improve the knowledge of the Meloidae species of southeastern Iran, faunistic Accepted: 11 September, 2020 investigations on blister beetles of this region were carried out. Totally, 30 species belonging to 10 genera from two subfamilies (Meloinae and Published: Nemognathinae) were identified. Among the identified specimens, 22 species 14 September, 2020 were new for fauna of Kerman province. Subject Editor: Sayeh Serri Key words: Meloidae, Southeastern Iran, Meloinae, Nemognathinae, Fauna Citation: Nezhad-Ghaderi, S.S., Nozari, J., Badoei Dalfard, A. & Hosseini Naveh, V. (2021) List of species of blister beetles (Coleoptera: Meloidae) in Kerman province, Iran. Journal of Insect Biodiversity and Systematics, 7 (1), 1–13. -
Numerical Investigation of Groundwater Balance and Artificial Recharge in the Kerman-Baghin Aquifer
Journal of Hydraulic Structures J. Hydraul. Struct., 2021; 7(2):1-21 DOI: 10.22055/jhs.2021.36940.1166 Numerical investigation of groundwater balance and artificial recharge in the Kerman-Baghin Aquifer Sina Pakmanesh 1 Mahnaz Ghaeini-Hessaroeyeh 2 Ehsan Fadaei-Kermani 3 Abstract In the present paper, the behavior of Kerman-Baghin aquifer has been investigated using the MODFLOW program and GMS 10.3 software. The piezometer data during October 2011 are applied for steady state condition of groundwater modeling. Then, the model is calibrated for 66 months for unsteady condition using observational information, and it is validated for 24 months. Finally, the results are compared with the available observed data and show acceptable accuracy in calibration and validation steps. After validating the model, the status of the aquifer is estimated for a period of 5 years. Management scenarios including 10, 20 and 30 percent reduction in groundwater abstraction as well as artificial recharge at eight selected aquifer sites have been investigated. The location of artificial recharge sites is selected based on seven parameters of land slope, distance from waterways, distance from faults, electrical conductivity, hydraulic conductivity, geology of the area and groundwater depth (thickness of unsaturated area). These parameters are combined with the index overlay method by Arc GIS 10.3 software. The results show that by continuing the current situation, the Kerman-Baghin aquifer could face an average annual deficit of more than 52 million cubic meters. It may cause various problems in the near future including abstraction water from groundwater sources and reducing water quality. The results of implementing different scenarios show that, the best scenario can be obtained by 10% reducing water withdrawal with artificial recharge in four zones 1, 2, 10 and 12. -
Of SE Iranian Mountains Exemplified by the Kuh-I-Jupar, Kuh-I-Lalezar and Kuh-I-Hezar Massifs in the Zagros
Umbruch 77.2-3 09.12.2008 15:43 Uhr Seite 71 Polarforschung 77 (2-3), 71 – 88, 2007 (erschienen 2008) The Pleistocene Glaciation (LGP and pre-LGP, pre-LGM) of SE Iranian Mountains Exemplified by the Kuh-i-Jupar, Kuh-i-Lalezar and Kuh-i-Hezar Massifs in the Zagros by Matthias Kuhle1 Abstract: Evidence has been provided of two mountain glaciations in the tion the Kuh-i-Lalezar massif (4374 m, 29°23'28.01" N 4135 m high, currently non-glaciated Kuh-i-Jupar massif in the semi-arid 56°44'49.38" E) has been visited in April and May 1973. The Zagros: an older period during the pre-LGP (Riss glaciation, c. 130 Ka) and a younger one during the LGP (Würm glaciation, Marine Isotope Stage (MIS) results attained by Quaternary geological and geomorpholo- 4-2: 60-18 Ka). During the pre-LGP glaciation the glaciers reached a gical methods stand in contrast to earlier assumptions concern- maximum of 17 km in length; during the LGP glaciation they were 10-12 km ing the former glaciation of these semi-arid Iranian mountains. long. They flowed down into the mountain foreland as far as 2160 m (LGP glaciation) and 1900 m (pre-LGP glaciation). The thickness of the valley Parts – Kuh-i-Jupar massif – were already published in glaciers reached 550 (pre-LGP glaciation) and 350 m (LGP glaciation). German. They are included in this paper in a summarized During the pre-LGP a 23 km-wide continuous piedmont glacier lobe devel- form. In continuation of these results new observations from oped parallel to the mountain foot.