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سال سيزدهم، شماره 8، تابستان 0260 تحقيقات منابع آب ايران Volume 13, No. 2, Summer 2017 (IR-WRR) Iran-Water Resources Research 199-236 يادداشت فنی Technical Note استخراج منحنیهای عمق- مساحت- تداوم بهمنظور Derivation of Depth- Area- Duration Curves for Estimating Areal Probable Maximum برآورد حداکثر بارش محتمل منطقهای در استان فارس Precipitation in Fars Province 2 *8 0 زهرا جهانديده ، بهرام بختياری و کوروش قادری Z. Jahandideh 2, B. Bakhtiari2* and K. Qaderi3 چکيده Abstract حداکثر بارش محتمل بزرگترين عمق بارش در يک تداوم معين و ممکن Probable Maximum Precipitation is the greatest depth of است. در اين مطالعه، استخراج منحنيهای عمق- مساحت- تداوم )precipitation for certain duration. This study aimed derivation )DAD of Depth-Area-Duration (DAD) curves in Fars province for PMP24 جهت برآورد حداکثر بارش محتمل 24 ساعته ) ( با استفاده از دو (estimating 24-h Probable Maximum Precipitation (PMP24 نگرش آماری هرشفيلد و برآورد عامل فراواني )km( مناسب در استان فارس using two Hershfield statistical approaches and estimating the suitable frequency factor (km). For these purposes the مدنظر ميباشد. بهاينمنظور از دادههای حداکثر باران 24ساعته )P24)max)( maximum 24-hour precipitation data ((P24)max) with a period با دوره آماری 12 تا 61 سالهی 52 ايستگاه واجد آمار طوﻻنيمدت واقع در of 12-61 years were obtained for 52 stations with long-term اين استان استفاده گرديد. مقادير km در نگرش اول و دوم بهترتيب، در data. The km values in the first and second approaches were estimated between 15.3 to 18.4 and 1.6 to 6.8, respectively. محدوده 4/18- 0/15 و 8/6- 6/1 و PMP24 متناظر در محدوده -853 Also the corresponding PMP24 were between 280 to 850 and 283 و 083- 112 ميليمتر برآورد شدند. مقادير PMP24 با دوره to 380 mm respectively for the two approaches. The 112 بازگشتهای 53 و 133 سال بهترتيب 714 و 771 ميليمتر محاسبه گرديد. PMP24 values were estimated of 50 and 100 year return periods 714 and 771 mm, respectively. Results showed that نتايج نشاندهنده کاهش 75 درصدی km نگرش دوم نسبت به نگرش اول the km values for the second approach are 75% lower than the (P24)max PMP24 در منطقه مطالعاتي ميباشد. نسبت به در نگرش اول و km for the first approach. The ratios of PMP24 to (P24)max were دوم بهترتيب 4/7-6/2 و 7/2-4/1 بهدست آمد. لذا اطمينانپذيری نگرش obtained in the range of 2.6 to 7.4 and 1.4 to 2.7 respectively for the first and second approaches. Therefore, the second دوم نسبت به نگرش اول بيشتر ميباشد. همچنين نقشههای هممقدار approach is more reliable. Also, the isohyet maps were drawn PMP24 در منطقه مطالعاتي برای دو نگرش با استفاده از مدل رقومي for PMP for the two approaches over the study area using ارتفاع در محيط نرمافزاری ArcGIS 10.3 ترسيم و منحنيهای DAD و DEM in GIS. DAD and area reduction curves were determined for each approach. Using these curves it is کاهش سطح هريک از نگرشها تعيين شدند. کاربرد اين منحنيها تبديل possible to convert point PMP24 values to areal values in the PMP24 نقطهای به منطقهای را در استان فارس امکانپذير ميسازد. .Fars province کلمات کليدی: حداکثر بارش محتمل )PMP(، روش آماری، منحني ,(Keywords: Probable maximum precipitation (PMP Hershfield method, Area reduction curve, Frequency factor, کاهش سطح، عامل فراواني، استان فارس. .Fars province تاريخ دريافت مقاله: Received: May 21, 2016 95/0/1 تاريخ پذيرش مقاله: Accepted: July 14, 2016 95/4/24 1- دانشجوی کارشناسي ارشد مهندسي منابع آب؛ دانشکده کشاورزی؛ دانشگاه شهيد باهنر M. Sc. student in Water Resource Engineering, Water Engineering 1- کرمان؛ کرمان؛ ايران ,Department, Faculty of Agriculture, Shahid Bahonar University of Kerman 2- استاديار بخش مهندسي آب؛ دانشکده کشاورزی؛ دانشگاه شهيد باهنر کرمان؛ کرمان؛ .Kerman, Iran 2- Assist Professor, Water Engineering Department, Faculty of Agriculture, ايران :Shahid Bahonar University of Kerman, Kerman, Iran, Email 0- دانشيار بخش مهندسي آب؛ دانشکده کشاورزی؛ دانشگاه شهيد باهنر کرمان؛ کرمان؛ [email protected] ايران ,Associate Professor, Water Engineering Department, Faculty of Agriculture 3- *- نويسنده مسئول .Shahid Bahonar University of Kerman, Kerman, Iran بحث و مناظره (Discussion) در مورد اين مقاله تا پايان پاييز 1096 امکانپذير است. Corresponding Author -* 199 PMP 0- مقدمه با توجه به اينکه در مطالعات گذشته برآورد بصورت نقطهای انجام شده و اثر گراديان بارش و منحنيهای کاهش سطح در آن بارش در بين عناصر اقليمي از اهميت بسيار زيادی برخوردار است لحاظ نشده است. هدف مطالعه حاضر بررسي توزيع مکاني بارش، )Ros et al., 2008( به گونهای که يکي از مسائل مهم در طراحي ترسيم منحنيهای DAD، استخراج منحنيهای کاهش سطح و سازههای آبي برآورد حداکثر بارش محتملPMP( 1( است. PMP به برآورد منطقهای حداکثر بارش محتمل در ايستگاههای باران-سنجي عنوان داده ورودی اوليه برای محاسبات سيﻻب طراحي که و سينوپتيک منطقه مطالعاتي تعريف شده است. اساس طراحي سازههای آبي است، دارای اهميت ميباشد )PMP .)Ros et al., 2008 برابر بيشترين ارتفاع بارشي است که امکان رخداد آن از نظر فيزيکي در يک محدوده جغرافيايي و در يک 8- مواد و روشها زمان معين از سال وجود داشته باشد )WMO, 2009(. بهمنظور 8-0- منطقه مطالعاتی و دادهها برآورد منطقهای PMP و کسب آگاهي از تغييرات مکاني بارش، استان فارس با مساحت 122638 کيلومتر مربع بين طولهای 2 روابط عمق- سطح- تداوم )DAD( بررسي ميشوند. منظور از جغرافيايي ´06˚53 تا ´05˚55 شرقي و عرضهای جغرافيايي بررسي DAD ترتيب دادن اطﻻعاتي است که به سهولت بتوان به ´30˚27 تا ´43˚01 شمالي واقع شده است. استان فارس بر اساس حداکثر مقدار بارش در بخشي يا تمامي حوضه آبخيز در مدت طبقهبندی اقليمي دومارتن گسترشيافته به پنج ناحيه اقليمي خشک زمانهای مختلف بارش رگبار دست يافت. با استفاده از منحنيهای معتدل، نيمهخشک معتدل، خشک سردسير، نيمهخشک سردسير و عمق- مساحت- تداوم و تجزيه بارندگي به ازای سطوح مختلف خشک گرمسير طبقهبندی ميشود. در اين مطالعه از دادههای 52 حوضه، مقدار بيشينه بارندگي در پايههای زماني متفاوت تعيين ايستگاه سينوپتيک و بارانسنجي اخذ شده از اداره کل هواشناسي ميگردد. بر اساس منحنيها يا روابط DAD ميتوان ميانگين بيشينه استان فارس و شرکت آب منطقهای استان فارس استفاده شد. در بارندگي را برای هر سطحي از حوضه که فاقد ايستگاه باشد به دست جدول 1 مشخصات جغرافيايي و در شکل 1 محدوده منطقه مطالعاتي آورد )Ghafourian and Telvari, 2010(. تاکنون برای مناطقي از و محل ايستگاههای منتخب آورده شده است. ايران و ساير نقاط دنيا محاسبات حداکثر بارش محتمل 24 ساعته k صورت گرفته است. مقادير m برای تعدادی از نمونههای اقليمي 8-8- روشها ايران تصحيح گرديد و تأثير طول دوره آماری بر فاکتور فراواني هرشفيلد بر مبنای وجود سری ساﻻنه دادههای بارش با تداوم مورد بررسي شد )Bakhtiari, 1999(. از جمله ديگر مطالعات ميتوان به نظر در نقاط مشاهدهای روشي را جهت برآورد PMP ارائه کرد برآورد حداکثر بارش محتمل بــه روش آماری در استان فارس )Hershfield, 1961; Hershfield, 1965(. اساس آن معادله Parsamehr et al. , 2014; Mansouri and Boostani, 2010; ( عمومي تناوبِ ارائه شده توسط (Chow (1951 ميباشد و بهصورت Mazidi and Omidi, 2011(، استخراج منحنيهای DAD به معادله 1 تعريف ميشود. منـــظور محاسبه PMP در حــوضهای در کشــــور هلنـــد 푥푡 = 푥̅푛 + 푘푡휎푛 )1( )Kingpaiboon and Netwang( و حــوضه آجيچای که در آن 푥푡 حداکثر بارش ساﻻنه با دوره بازگشت 푡 سال، 푥̅푛 )Azizi and Hanafi, 2011(، اشاره کرد. (Desa et al. (2001 و متوسط بارش ساﻻنه، 휎푛 انحراف معيار برای بارشهای ساﻻنه و 푘푡 (Desa and Rakhecha (2007 روش هرشفيلد را بر اساس حداکثر عامل فراواني متناظر با دوره بازگشت سال است. بارش مشاهده شده مورد تجديد نظر قرار دادند که اين کار منجر به کاهش شديدی در ضريب فراواني گرديد و در مطالعه حاضر از اين هرشفيلد به اين نتيجه رسيد که در برآورد 푃푀푃 از يک عامل روش تحت عنوان نگرش دوم ياد ميشود. (Ghahraman (2008 فراواني نبايد تخطي کرد، بنابراين 푘푡 را با 푘푚 جايگزين کرد و به نــگرش تجــديـــد نظر يافتــــه هرشفيلد را برای حوضه اترک و دنبال آن 푥푡 نيز با 푃푀푃 تعويض ميشود، لذا معادله فوق به صورت (Afzali Gorouh et al. (2015 برای حوضه قرهسو در استان معادله )2( بازنويسي ميشود. گلستان و (Paymozd et al. (2005 آن را برای حوضههايي در 푃푀푃 = 푥̅ + 푘푚휎푛 )2( شرق استان هرمزگان بهکار بردهاند و نگرش دوم را پيشنهاد کردند. تحقيقات منابع آب ايران، سال سيزدهم، شماره 8، تابستان 0260 Volume 13, No. 2, Summer 2017 (IR-WRR) 233 Table 1- Geographical characteristics of selected stations for PMP calculation in Fars province جدول 0- مشخصات ايستگاههای منتخب جهت محاسبه PMP در استان فارس Altitude Length of Latitude Longitude Station type Station from sea record (N) (E) level (m) (year) Shiraz 29˚32′ 52˚36′ 1484 61 Fasa 28˚58′ 53˚41′ 1288 50 Abadeh 31˚11′ 52˚40′ 2030 40 Zarghan 29˚47′ 52˚43′ 1596 34 Dorudzan 30˚11′ 52˚17′ 1650 29 Lar 27˚42′ 54˚17′ 792 27 Synoptic Eghlid 30˚54′ 52˚38′ 2300 23 Darab 28˚47′ 54˚17′ 1098 22 Lamerd 27˚22′ 53˚12′ 405 22 Neyriz 29˚12′ 54˚20′ 1632 17 Bavanat 30˚28′ 53˚40′ 2231 14 Takhte Jamshid 29˚56′ 52˚54′ 1605 14 Jahrom 28˚29′ 53˚32′ 1082 12 Abadeh tashk 29˚48′ 53˚43′ 1604 42 Ahmadabad 30˚23′ 52˚41′ 2233 48 Arsenjan 29˚55′ 53˚19′ 1648 42 Estahban 29˚07′ 54˚04′ 1755 28 Emamzade 30˚19′ 52˚35′ 1842 29 Poltalkh 29˚27′ 53˚25′ 1592 26 Jamalbeig 30˚36′ 51˚57′ 2010 46 Jahanabad 29˚42′ 53˚51′ 1577 44 Chamriz 30˚47′ 52˚10′ 1840 45 Chubkhale 30˚32′ 51˚53′ 2056 42 Hosseinabad 29˚57′ 52˚21′ 1695 41 Kharame 29˚29′ 53˚19′ 1597 23 Khosroshirin 30˚54′ 52˚00′ 2340 27 Khelar 29˚57′ 52˚14′ 2078 22 Dorudzan 30˚21′ 52˚44′ 1662 31 Dezhkord 30˚43′ 51˚57′ 2107 22 Dashtbal 30˚00′ 52˚58′ 1673 45 Dashtak 30˚17′ 52˚28′ 2031 30 Doshmanziari 30˚04′ 52˚22′ 1615 22 Raingauge Dehbid 30˚39′ 53˚11′ 2312 42 Dehkade sefid 30˚42′ 52˚04′ 2181 39 Dubane 29˚25′ 52˚46′ 1490 41 Sade 30˚43′ 52˚09′ 2192 25 Sarvestan 29˚16′ 53˚13′ 1570 36 Sahlabad 29˚15′ 53˚53′ 1518 27 Shul 29˚44′ 52˚48′ 1620 22 Edare markazi 29˚37′ 52˚32′ 1522 47 Fenjan 30˚23′ 53˚29′ 2376 21 Ghatre aghaj 30˚43′ 51˚53′ 2306 43 Ghalat 29˚50′ 52˚20′ 1881 41 Kaftar 30˚31′ 52˚43′ 2350 34 Katuri 29˚59′ 53˚21′ 2003 42 Komehr 30˚27′ 51˚52′ 2377 18 Garde Estahban 29˚09′ 53˚52′ 1698 21 Goshnegan Maharlu 29˚30′ 52˚52′ 1450 24 Madarsoleiman 30˚19′ 53˚18′ 1868 26 Mehrabad 29˚58′ 52˚42′ 1616 42 Neyriz 29˚11′ 54˚20′ 1657 36 Haragan 29˚06′ 54˚28′ 1898 47 تحقيقات منابع آب ايران، سال سيزدهم، شماره 8، تابستان 0260 Volume 13, No.
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  • The Political and Martial Role of the Fars Ethnic Groups in the Qajar Period Until the Constitutionalism Epoch; with Emphasis on the “Qashqaee Tribe”

    The Political and Martial Role of the Fars Ethnic Groups in the Qajar Period Until the Constitutionalism Epoch; with Emphasis on the “Qashqaee Tribe”

    J. Appl. Environ. Biol. Sci., 4(8)16-22, 2014 ISSN: 2090-4274 Journal of Applied Environmental © 2014, TextRoad Publication and Biological Sciences www.textroad.com The Political and Martial Role of the Fars Ethnic Groups in the Qajar Period until the Constitutionalism Epoch; with Emphasis on the “Qashqaee Tribe” Ali Akbar Safipur1., Reza Sheybani2 1,2 Department of History, College of Humanities & Social Science, Tehran Science and Research Branch, Islamic Azad University, Tehran, Iran Received: May 22, 2014 Accepted: July 30, 2014 ABSTRACT In a territory based upon geographical and influential climatic formations, one- third of its soil was in possession of ethnic groups or clans, who were within their own bounds of tribal life, having their special logic. Moreover, founded on acceptable public roles, they ranked in acting as a completely unified aggregate. Conditions and the state of affairs of ethnic groups in the country, in the recent decades of the 19th Century; and particularly, in regions where from archaic times, until date, powerful ethnic groups were present. These clans displayed their capabilities to conserve their internal tribal consolidation and its vital role, in the vast expanse of the political and economic fate of the country and throughout the land. Emphasis and inclination as to the minor capacities, such as the Fars ethnic groups in the 19th Century, institutionalized in determining the regional and local policies. This also denotes the stance where their political and social structure was extremely in coherence and played an outstanding role in the public destinies of the country and that, which has even remained in the Middle East.
  • Diptera: Tachinidae) from Fars Province, Iran

    Diptera: Tachinidae) from Fars Province, Iran

    Turk J Zool 34 (2010) 35-43 © TÜBİTAK Research Article doi:10.3906/zoo-0805-10 A contribution to the tachinid flies of the subfamilies Exoristinae and Tachininae (Diptera: Tachinidae) from Fars province, Iran Mehdi GHEIBI1,*, Hadi OSTOVAN2, Karim KAMALI1 1Department of Entomology, Islamic Azad University, Science and Research Branch, Tehran - IRAN 2Department of Entomology, Islamic Azad University, Fars Science and Research Branch, Marvdasht - IRAN Received: 21.05.2008 Abstract: Data are given on the distribution of 40 species belonging to the subfamilies Exoristinae and Tachininae that were collected by the first author in Fars province, Iran, during 2006-2007. In all, 22 species were recorded for the first time from Iran and 34 species from Fars province. Erynniopsis antennata (Rondani, 1861) was reared for the first time on the host Diorhabda elongate (Coleoptera: Chrysomelidae). Key words: Diptera, Tachinidae, Iran, Fars, distribution Introduction The most reliable characters for recognizing a The family Tachinidae forms the largest and one tachinid fly are the presence of hypopleural (meral) of the most diverse families of flies (Diptera, bristles and the well-developed sub-scutellum. Brachycera). Worldwide, this family comprises more Members of the family are often conspicuously bristly, than 8000 described species in 4 subfamilies: whilst others, especially many species from the Exoristinae, Tachininae, Dexiinae, and Phasiinae subfamily Phasiinae, are often quite bare. The larvae (Herting, 1984). The actual number of the family is live as endoparasitoids in Arthropoda, almost much larger, as the Neotropical, Afrotropical, exclusively in insects. Insects known as tachinid hosts Oriental, and Australasian regions are not well studied belong to 11 orders, and Lepidoptera caterpillars serve and contain large numbers of undescribed species as hosts for the majority of species.
  • Note on the Presidential Election in Iran, June 2009 Walter R. Mebane

    Note on the Presidential Election in Iran, June 2009 Walter R. Mebane

    Note on the presidential election in Iran, June 2009 Walter R. Mebane, Jr. University of Michigan June 24, 2009 (updating report originally written June 14 and updated June 16, 17, 18, 20, 22 & 23) The presidential election that took place in Iran on June 12, 2009 has attracted con- siderable controversy. The incumbent, Mahmoud Ahmadinejad, was officially declared the winner, but the opposition candidates—Mir-Hossein Mousavi, Mohsen Rezaee and Mehdi Karroubi—have reportedly refused to accept the results. Widespread demonstrations are occurring as I write this. Richard Bean1 pointed me to district-level vote counts for 20092 This URL has a spread- sheet containing text in Persian, a language I’m unable to read, and numbers. I know nothing about the original source of the numbers. Dr. Bean supplied translations of the candidate names and of the provinces and town names. There are 366 observations of the district (town) vote counts for each of the four candidates. The total number of votes recorded in each district range from 3,488 to 4,114,384. Such counts are not particularly useful for several of the diagnostics I have been studying as ways to assess possible problems in vote counts. Ideally vote counts for each polling station would be available. (added June 17) Shortly after I completed the original version of this report, Dr. Bean sent me a file, supposedly downloaded from the same source, containing district-level vote counts for the second round of the 2005 presidential election. The candidates in that contest were Mahmoud Ahmadinejad and Akbar Hashemi Rafsanjani.
  • Water and Water Shortage in Iran Case Study Tashk-Bakhtegan and Maharlu Lakes Basin, Fars Province, South Iran

    Water and Water Shortage in Iran Case Study Tashk-Bakhtegan and Maharlu Lakes Basin, Fars Province, South Iran

    Water and water shortage in Iran Case study Tashk-Bakhtegan and Maharlu lakes basin, Fars Province, South Iran vorgelegt von M. Sc. Fatemeh Ghader geb. in Shiraz von der Fakultät VI - Planen Bauen Umwelt der Technischen Universität Berlin zur Erlangung des akademischen Grades Doktor der Ingenieurwissenschaften – Dr.-Ing. – genehmigte Dissertation Promotionsausschuss: Vorsitzender: Prof. Dr. Tomás Manuel Fernandez-Steeger Gutachter: Prof. Dr. Uwe Tröger Gutachter: Prof. Dr. Michael Schneider Tag der wissenschaftlichen Aussprache: 10. August 2018 Berlin 2018 To my husband who supported me and light up my life Abstract Tashk-Bakhtegan and Maharlu lakes' basin in Fars province in south of Iran is facing a harsh water shortage in recent years. Semi-dry and dry conditions are prevailing climate conditions in the basin and the wet condition can only be seen in the small part of the north. Groundwater is the main source to provide water for different purposes such as agriculture, industry and drinking. Over-exploitation of water more than aquifers potential caused exploitation of prohibited water and prevailing the critical condition in vast part of basin. Kor and Sivand rivers are the only permanent rivers in the basin and they flow only in some parts of basin and they supply part of the water demand. Some factors such as geological setting, the rate of evaporation, existence of two salt lakes and Salt Lake's intrusion from the lakes has caused a decrease in water quality especially in the south of the basin. In this study for the first time a complete research was carried out to understand the hydrologic circle of Tashk-Bakhtegan and Maharlu lakes' basin.
  • Geomorphic Signatures of Active Tectonics of Darian Area, Northeast of Shiraz, Iran

    Geomorphic Signatures of Active Tectonics of Darian Area, Northeast of Shiraz, Iran

    J. Bio. & Env. Sci. 2015 Journal of Biodiversity and Environmental Sciences (JBES) ISSN: 2220-6663 (Print) 2222-3045 (Online) Vol. 7, No. 1, p. 572-578, 2015 http://www.innspub.net RESEARCH PAPER OPEN ACCESS Geomorphic Signatures of Active Tectonics of Darian Area, Northeast of Shiraz, Iran Mahdi Azadmanesh1*, Mohsen Pour kermani1, Abdolmajid Asadi2, Manouchehr Ghorashi1, Ali Solgi3 1Department of Geology, North Tehran Branch, Islamic Azad University, Tehran. Iran 2Department of Geology, Shiraz Branch, Islamic Azad University, Shiraz, Iran 3Department of Geology, Science and Research Branch, Islamic Azad University, Tehran. Iran Article published on July 30, 2015 Key words: Geomorphic, Active Tectonics, Darian, Shiraz. Abstract This paper examines both the relative Active Tectonics of Gadvan anticline based on morphometric parameters and their application in morphology and topography evolution in northeast of Shiraz. In the present study, the analysis including line ament mapping, length density mapping, intersection and the counts of lineaments and also the calculation of three geomorphic parameters (Smf, facet% and Vf) have been conducted. Some of which can be used in the study of morphology. According to the classification of geomorphic indicators, the study area was tectonically detected as an area within tense activity. Therefore, the uplift rate in this area is over the front of the mountain which is estimated about 1/5 to 4 mm per year. In the study, for the extraction of lineaments, automatic and semi-automatic methods along with manual one werealso conducted. Area lineament maps and length density, counts not only specifies areas with anomalous fracture but also can contribute in determining the location of drilling water wells of Darian plains.
  • Folding Pattern in the Fars Province, Z

    Folding Pattern in the Fars Province, Z

    Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Solid Earth Discuss., 7, 2347–2379, 2015 www.solid-earth-discuss.net/7/2347/2015/ doi:10.5194/sed-7-2347-2015 SED © Author(s) 2015. CC Attribution 3.0 License. 7, 2347–2379, 2015 This discussion paper is/has been under review for the journal Solid Earth (SE). Folding pattern in the Please refer to the corresponding final paper in SE if available. Fars province Folding pattern in the Fars province, Z. Maleki et al. Zagros folded belt: case study on the Title Page Karbasi and Khaftar anticlines, interior Abstract Introduction Fars, Iran Conclusions References Tables Figures Z. Maleki, M. Arian, and A. Solgi Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran J I Received: 25 July 2015 – Accepted: 28 July 2015 – Published: 17 August 2015 J I Correspondence to: M. Arian ([email protected]) Back Close Published by Copernicus Publications on behalf of the European Geosciences Union. Full Screen / Esc Printer-friendly Version Interactive Discussion 2347 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract SED The anticlines in Fars region, which are located in Zagros fold-thrust belt, are valu- able because they possess several hydrocarbons and this area is easily recognized by 7, 2347–2379, 2015 the NW–SE trending parallel anticlines that verge to the SW. According to the geolog- 5 ical classification, the study area is located in Interior Fars region. Due to increasing Folding pattern in the complication of structural geometry in Fars region and necessity to explore activities Fars province for deeper horizons especially the Paleozoic ones, the analysis of fold style elements, which is known as one of the main parts in structural studies, seems necessary.
  • Journal of Neolithic Archaeology

    Journal of Neolithic Archaeology

    Journal of Neolithic Archaeology 4 May 2020 doi 10.12766/jna.2020.1 Kutahi: A Pottery Neolithic Culture on the Shiraz Article history: Plain, Fars, Iran Received 26 August 2018 Reviewed 30 December 2018 Majid Mansouri Published 4 May 2020 Keywords: Kutahi, Pottery Neolithic, Fars, Abstract Shiraz, Museum collection The British Council in Shiraz was established in 1960 and Paul Cite as: Majid Mansouri: Kutahi: A Pottery Bevan Gotch was appointed as its regional director until 1966. Dur- Neolithic Culture on the Shiraz Plain, Fars, Iran ing this time, he regularly met, hosted and corresponded with ar- JNA 22, 2020, 1 – 14 [doi 10.12766/jna.2020.1] chaeologists working in the Fars region. These relationships as well as the reports of the archaeological fieldworks conducted on the Fars, Author‘s address: especially in the Kor River Basin, inspired Gotch to do some region- Majid Mansouri al surveys on the Persepolis and Shiraz plains. He identified a total Independent researcher of six prehistoric sites on the Shiraz plain, of which the site of Kutahi Firuzabad, Fars, Iran was one of the most important. As Gotch mentioned this site as being [email protected] ploughed and regularly bulldozed during his surveys, it is likely that it was later levelled and subsequently vanished forever due to the growth of the city of Shiraz. However, Gotch collected some sherds during his 1966 survey and also during a repeated visit in 1972. The location of the 1966 survey collection is unclear, but the 1972 collec- tion is kept at the Narenjestan museum in Shiraz.