The Study on Reconstruction Plan for Bam Water Supply System
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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. -
Petrology and the Origin of the Intrusive Masses of the East of Jiroft
Revista Geoaraguaia ISSN:2236-9716 Barra do Garças - MT v.9, n.2, p.22-36. Agosto 2019 PETROLOGY AND THE ORIGIN OF THE INTRUSIVE MASSES OF THE EAST OF JIROFT PETROLOGIA E ORIGEM DE MATERIAIS INTRUSIVOS NO LESTE DE JIROFT Farbod Faraji Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran Afshin Ashja-Ardalan Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran [email protected] Moosa Kalimi-Noghreeian Department of Geology, Isfahan University, Isfahan, Iran Hamidreza Jafari Department of Geology, Sirjan Branch, Islamic Azad University, Sirjan, Iran ABSTRACT The study area with an area of 55 km2 is located south east of Kerman province and in the area of Jiroft city. This area is structurally and geological division in the Urmia-Dokhtar zone. The Urmia- Dokhtar volcanic belt part of the Alpine-Himalayan is a volcanic belt. Several intrusive bodies are in the east of Jiroft, which is part of Jebalbarez Batolite andigneous actives of JabalBarez area have occurred in four stages. The third magma activity of the region occurred in Oligomiocene and occurred during three phases. its lithological composition includes synogranite and Monzogranite, granodiorite, diorite, quartz monzonite. Quartz, Plagioclase and Potassium feldspar are the major minerals in granites. Biotite, Amphibole, espen, opac minerals are other manufactores of these rocks. Various types of granular, myrmekitic, Graphic and perthite textures are observed in them. Regarding field studies, petrographic, and geochemical studies, granite rocks of meta-aluminum and granitoid components of Iseries are volcanic arc of the continental margin of orogenic region that originate from melting of shell-shaped igneous rocks. -
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. -
And “Climate”. Qarah Dagh in Khorasan Ostan on the East of Iran 1
IRAN STATISTICAL YEARBOOK 1397 1. LAND AND CLIMATE Introduction T he statistical information that appeared in this of Tehran and south of Mazandaran and Gilan chapter includes “geographical characteristics and Ostans, Ala Dagh, Binalud, Hezar Masjed and administrative divisions” ,and “climate”. Qarah Dagh in Khorasan Ostan on the east of Iran 1. Geographical characteristics and aministrative and joins Hindu Kush mountains in Afghanistan. divisions The mountain ranges in the west, which have Iran comprises a land area of over 1.6 million extended from Ararat mountain to the north west square kilometers. It lies down on the southern half and the south east of the country, cover Sari Dash, of the northern temperate zone, between latitudes Chehel Cheshmeh, Panjeh Ali, Alvand, Bakhtiyari 25º 04' and 39º 46' north, and longitudes 44º 02' and mountains, Pish Kuh, Posht Kuh, Oshtoran Kuh and 63º 19' east. The land’s average height is over 1200 Zard Kuh which totally form Zagros ranges. The meters above seas level. The lowest place, located highest peak of this range is “Dena” with a 4409 m in Chaleh-ye-Loot, is only 56 meters high, while the height. highest point, Damavand peak in Alborz The southern mountain range stretches from Mountains, rises as high as 5610 meters. The land Khouzestan Ostan to Sistan & Baluchestan Ostan height at the southern coastal strip of the Caspian and joins Soleyman Mountains in Pakistan. The Sea is 28 meters lower than the open seas. mountain range includes Sepidar, Meymand, Iran is bounded by Turkmenistan, the Caspian Sea, Bashagard and Bam Posht Mountains. -
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. -
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. -
Microbiostratigraphy of the Lower Cretaceous Strata from the Bararig Mountain, SE Iran
Revista Mexicana de CienciasMicrobiostratigraphy Geológicas, v. of 29, the núm. Lower 1, 2012,Cretaceous p. 63-75 strata from the Bararig Mountain SE Iran 63 Microbiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iran Mahin Rami1, Mohammad Reza Vaziri2, Morteza Taherpour Khalil Abad3,*, Seyed Abolfazl Hosseini4, Ivana Carević5, and Mohsen Allameh6 1 Department of Geology, North-Tehran Branch, Islamic Azad University, Tehran, Iran. 2 Shahid Bahonar Universty, Kerman, Iran. 3 Department of Geology, Mashhad Branch, Islamic Azad University, Mashhad, Iran. Young Researchers Club, Mashhad Branch, Islamic Azad University. 4 Exploration Directorate, National Iranian Oil Company, Tehran, Iran. 5 Faculty of Geography, University of Belgrade, Studentski trg 3/3, 11000 Belgrade, Serbia. 6 Department of Geology, Mashhad Branch, Islamic Azad University, Mashhad, Iran. * [email protected] ABSTRACT The Barremian-Aptian sediments in the Bararig section (Southwest of Kuhbanan) consist of an alternation of marl and limestone. The palaeontological analysis led to identification of twenty seven taxa of benthic foraminifera and algae in the section studied. Diverse assemblages of benthic foraminifera and also the low planktonic/benthic (P/B) ratio show that the sedimentary environment in the study area was oxygenated and shallow. Key words: microbiostratigraphy, palaeoecology, Lower Cretaceous, Bararig section, Kerman Province, Iran. RESUMEN Los sedimentos del Barremiano-Aptiano en la sección Bararig section (al suroeste de Kuhbanan) consisten en una alternancia de margas y calizas. El análisis paleontológico permitió la identificación de 27 taxa de foraminíferos bentónicos y algas en la sección estudidad. Diversas asociaciones de foraminíferos bentónicos y la baja relación de planctónicos/bentónicos (P/B) indica que el ambiente sedimentario en el área de estudio fue oxigenado y somero. -
Enresume.Mjmalakouti.Pdf
"IN THE NAME OF ALMIGHTY" Curriculum Vitae (C. V.) Personal Data Mohammad Jafar Malakouti Born on Dec. 12, 1947, Marand, Iran. Married since 1972 with two children. Education Ph.D. in Soil Sci., University of Nebraska, USA, 1977. M.Sc. in Soil Sci., University of Tehran, Iran, 1973. B.Sc. in Soil and Water Sci., University of Ahwaz, Iran, 1970. Language Persian, Turkish, and English Experiences: 2000- Present: Member of Council, Farmers' Union (NGO) and Honorary Consultant to to the Fertilizer Producers Association in Iran (NGO), Tehran, Iran. 1995 to 2011: Professor, Plant Nutrition, Soil Fertility and Fertilizers and Head of Soil Sci. Dept., Tarbiat Modares University (Graduate School). 1995 to 2006 Professor and Director General, Soil and Water Research Institute. Executive Committee Member, International Plant 2001 to 2010: Nutrition Society. 1988 to 2011: Head of Soil Sci. Dept., Tarbiat Modares University (Graduate School). 1996 to 2001: Advisor to the Minister of Agriculture. 1996 to 2005: Member, High Council of Policy Making on the Development of Biological Products, Optimum Utilization of Chemical Fertilizers and Pesticides. 1995 to 2005: Member, High Council for Water Commission, Ministry of Energy. 1994 to 2003: Board Member, Iranian Soil Sci. Society 1988 to 1995 : Associate Professor, Soil Sci. Dept. (Plant Nutrition, Soil Fertility). 1985 to 1988: Associate Professor, Soil Sci. (Soil Fertility, Plant Nutrition …), and Director General, Evaluation Office for Foreign Documents and Univiversity Degrees, Ministry of Sci. and Higher Education. 1982 to 1985: Assistant prof., Soil Sci. and Vice Chancellor, Tarbiat Modares Univ. 1980 to 1981 : Assistant Prof. and Dean of Zanjan Agricultural College, Zanjan, Iran. -
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. -
Abstract Book 2018.Pdf
Abstracts of Royan International Twin Congress 14th Congress on Stem Cell Biology and Technology 29-31 August 2018 Royan Institute Cell Science Research Center Tehran, Islamic Republic of Iran Scientif ic Board Abroun S. Aghdami N. Abstracts of the 14th Congress on Amini Nik S. Stem Cell Biology and Technology (2018) Ali Moghaddam K. Atari M. Contents: Baghban Eslami Nejad M. ● Collaborators ...................................................................... 3 Baharvand H. ● Chairman Wellcome Message ............................................ 5 Bahrami AR. ● Invited Speakers ................................................................. 6 Baradaran-Rafiee A. Bonakdar, SH ● Oral Presentations ............................................................ 16 Cohen-Tannoudji M. ●Poster Presentations .......................................................... 20 Dargahi L. ● Authors Index ................................................................... 52 Didar T. Ebrahimi M. Farzaneh F. Congress President: Gargett C. Fathi R, Ph.D Ghaedi K. Congress Chairperson: Gheraati M.R. Pahlevan S, Ph.D Hamidieh A.A. Hassani N. Committees Heydari S. Organizing Committee: Hosseini Salekdeh GH. Abdollahian E., B.Sc Javan M. Afsharian P., Ph.D Kageyama R. Ahmadi SE., M.Sc Kazemnejad S. Alizadeh SK., B.Sc Khademhosseini A. Azimi R., M.Sc Baharvand H., Ph.D Kemler R. Daliri L., M.Sc Kiani S. Ezabadi Z., M.Sc Kim J. Farrokh S., B.Sc Larijani B. Fathi R., Ph.D Malekzadeh R. Irani Sh., Ph.D Moghaddam MM. Kashfi F., M.Sc Lotfipanah M., M.Sc Moghaddasali R. Pahlevan S., Ph.D Mano JF. Shahverdi AH., Ph.D Mozafari M. Shahzadeh Fazeli A., Ph.D Niknejad H. Shiva M., MD Najimi M. Tavassolian R., B.Sc Samadi Kuchaksaraei A. Vosough M, MD., Ph.D Pahlavan S. Vosough Taghi Dizaj A., M.D Zarrabi M., M.D Prigione A. Rivron N. Executive Committee: Rouzafzoon R. -
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. -
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