DOCSLIB.ORG

Mercury Deposits in Turkey

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Mercury Deposits in Turkey SUJWEt f B 2 2 1979 Mercury Deposits in Turkey g GEOLOGICALSURVEYBULLETIN1456 G S Prepared in cooperation with s Maden Tetkik ve. Arama Enstitusii ><w O n o*o crq OJ no- Mercury Deposits in Turkey By MEHMET YILDIZ and EDGAR H. BAILEY GEOLOGICAL SURVEY BULLETIN 1456 Report prepared in cooperation with Maden Tetkik ve Arama Enstitusu Mineralogy, geologic setting, size-grade of mercury ore bodies; brief history of productive mines UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress catalog-card No. 78-600147 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-03134-5 CONTENTS Page Abstract -_-_._._._-_-_-_._._-_._._-_-_-_---_-_-_._-_-_---------_._._-- 1 Introduction ._._._._._-_._._._._._-_-_-_-_-_-----_-_._---_-_-----_---_ 1 Number and location of deposits .__----_-_ ._-_-_-_-_._-_-_-__-._ ._._ 2 History of mining -_-_-_-_---_-_-_-----_-_-----_-_-_-_---_---------_---- 3 Mercury deposits -_._-_-_._._-_-_---_-_-_---_-_-_-_-_-_----------__.--- 6 Geologic framework -_._._.___._---_-_-_-_ -_-_-_--.--_-___._-_-_-_ 6 Host rocks ____-_-_-___________---_-_-_---_-_-___-_-_-_-_---_-_-_-_ 10 Mineralogy ------------.-----.- ~------------------------^.------ 10 Size and grade ---_._..--...-._._._._._-_-___-_-_-_-_____._-_-_--._ 12 Origin and localization ._._._-_-_-_-_._-_-_-_-_-_-_._-_-_-_-_._.--_ 12 Descriptions of areas and mines -_-_-_-_-___---_-_-_-_-----_-_-_-------_ 14 Karaburun area -_._._._._ -_-_-_-_-_ -_-_-_-_ -_-_-_-,. 14 Karaburun mine (1) ._._.___---_-_-_-_-_-_-_-_._.--_-_-_._-_-_-_ 14 Karareis mine (2) ._._._._._-_-_---_-_-_-_-_._-_-_-_-_._._-_._-_ 20 Dikengik mind (3) -..-._ ._-.._..._._._._._._._._._._.___ 21 Tire area -_-_-_-_-_-_-_-_---_-_-_-_-_-_-_-_-_-_-_-_-_-_ ---_---_._ 23 Habibler mine (4) ._._._._-----_-_---_-_---_._._._..-.._..._._-- 24 Akmesc.it mine (5) .___._ ._-_.___._ -_._._ ._ ._._._ 24 Helvaci deposits (6) ._._._._-_._._._ -___-_-_._ -_._._ 26 Odemis. area -_-_-_-_,_._-_-_._-_-_-_-_---_-_-_._._-_._-----_-_-_-_ 26 Halikoy mine (7) .........----_._.-._.----.._.---_.-._.- .-.. 27 Tiirkomi mine (8) ._._._._._._._._._._._._._._._._._.. 30 Qamlica deposits (9) ._._._._._._-_-_-_-_._-_-_-_-_-_._-_._._._._ 32 Kahvedere deposit (10) ._ ....._......._._..............._.... 32 Salihli area ........ .. ._........ .... ..................... 32 Salihli deposits (11) ....._._..............._......._....._...... 35 Alagehir area -_-_-_-_-_._-_-_---_-_-_-_-_-_-_-_-_-_-_-_-_-_-_.- 35 Ala§ehir mine (12) ._._.___-_-_-_-_-_-_-_-_-_-_._._-_-_-_-_-_._ 35 Murat Dagi area -_-_-_-_-_-_._---_._-_---_-_-_-_._---_-_-_.___-_-_ 39 Baltali group (13) ............ ._..._.....__...... 40 Kestanelik Tepe mine (14) ._._._ __.__.,_._._.___-_-_ __ 44 Intepe mine (15) ._-_._-_._---_._-_-_-_-_-_-_._-_---_-_-_.--_-_ 45 Cigekli Kayasi Tepe mine (16) -_._-_-_-_-_-_._._-_-_.,____._._ 46 Agirsak Kayasi Tepe mine (17) ._-_._-_-_._-_-___._---_._-___._ 46 Karacahisar mine (18) -_-_---- -----_-_---_-_-_-_-_-_-_-_-_._-_ 47 Evrentdede deposits (19) ._._-_ -_-_-_ -_-_-_-_._._ -_.___ 50 Ivrindi area -_-_-_-_-_-_._-_-_-_-_-_-_-----_-_-_._._-_-_-_-_._-_-_-_ 50 Ivrindi occurrences (20) -__--_._-_-_-_-_-_-_._-_._-_-_-_._-_._-_ 50 Biga area -_-_-_-_-_-_._-_._-_._---_-_-_-_-_-_-_._-_-_-_---_-_-_._-_ 52 Hodul Koy mine (21) .......................................... 52 Izmit area -_-_-_-_-_-_..-_-_._-_-_._---_-_-_-_-_._-_._---_-_-_._-_ 53 Mudarli mine (22) ._._._._._._._._._._ ._._____._._._._.... 53 Sogiit area -_-_-_-_-_-_-_---_.___-_-_---_-_---_-_._._-_-_-___ --._ 55 Sbgiit occurrences (23) __._._ ._-_-___-_-_.___._._..___-_-_._-_._ 55 Inebolu area -_-_-_._-_-_-_-__--_-_-_-_-_-_-_-___-_-_-_-_-_-_..---_ 55 Seyhsaban mine (24) ._._- -_-_._-_-_-_-_._._-_-_._._-_._._ 56 ill iv CONTENTS Descriptions of areas and mines Continued Page Konya area -_-_-_-_-_-___-_-_-_.._-_-_-_____________________________ 57 Sizma mines (25) __-_-_-_-_-_____-_-___-___-___-_-_-___________ 59 Ladik mines (26) ____ --. .__-- ___ __ ______ 65 Nigde area ________________________________________________________ 72 Gumiisler mine (27) __._._._._._._._._._______.___._._._.___ 73 Mehmetleryurdu Sivrisi Tepe mine (28) ______ -_-_____-___ 77 Other deposits __-_-_-_-_-_-_-_-_____________-___-_-___________ 78 References cited _________________________________________________________ 78 ILLUSTRATIONS Page FIGURE 1. Map of Turkey showing location of mercury deposits -_-_____ 5 2. Graph showing mercury production in Turkey, 1906-74 .___ 7 3. Map of Turkey showing the relation of the mercury areas to the main structural provinces -___-_-_-_-_-_-_-_-_-_-_-_-_-___ 9 4. Map of the Karaburun Peninsula showing location of Karabu- run, Karareis, and Dikengik mercury mines ._-___-___-___ 14 5. Photograph of Karaburun mine viewed looking south ________ 16 6. Geologic map and cross section of the Karaburun (Kalecik) mine area __-_-_-_-_-_-_-_-_-_-_-___.._---_-_-_-_-_-_-_-_ 19 7. Photograph showing workers removing "burnt" ore from retorts at the Karaburun mine -_-_-_-___---_-_-_-_-_---_-_-_-_-_ 20 8. Generalized east-west section through Karareis mercury de­ posit ____-___-_-_._____________________-_-_-___.___ 22 9. Map of Tire area showing the location of the Habibler, Akmes- c,it, and Helvaci mercury mines -_-_-_---------___-_-----_ 23 10. Geologic map showing Akmesc.it mine and other mercury occur­ rences nearby -_-_-_-_-_-_-_-_-___---_-_-_-_-_---_-_-_-- 25 11. Map of the gneiss-schist contact from the Halikoy mine to the Kahvedere deposits ________._-_-_-_._- ._-_____-_-_._ 28 12. Map and section of Halikoy mine, 1964, from CENTO (1964) 29 13. Photograph of Halikoy furnace plant in 1966 ._-_-_-_-_._-_ 31 14. Map of the Qamlica mercury area _____--_-_-_-_---_-___---_ 33 15. Geologic map of the Kahvedere mercury area __-_._-_-_-_-_ 34 16. Geologic map of the area south of Alasehir showing the location of mercury and antimony deposits and outline of the Alasehir mine area -_-_-_______-_-___________-_-_-_-___._-_-_-_-_ 36 17. Geologic map of Ala§ehir mine area __---___-_-_-_-_-___---_ 37 18. Photograph of Alasehir mine camp and retort area ._-__--_-_ 38 19. Photograph showing bank of retorts in use at the Ala§ehir mine in 1966 ______________._-___-___._ -___________ 38 20. Map of the Murat Dagi area northwest of Banaz showing areas covered by geologic maps of mercury occurrences (figs. 22, 24, and 27) ._.______.__._._._._ __._._.___._._._ ._._._ 39 21.
Load more

Recommended publications
  • Download PDF About Minerals Sorted by Mineral Name
    MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky.
    [Show full text]
  • Overview of Tungsten Indicator Minerals Scheelite and Wolframite with Examples from the Sisson W-Mo Deposit, Canada
    Overview of tungsten indicator minerals scheelite and wolframite with examples from the Sisson W-Mo deposit, Canada M. Beth McClenaghan1, M.A. Parkhill2, A.A. Seaman3, A.G. Pronk3, M. McCurdy1 & D.J. Kontak4 1Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada K1A 0E8 (e-mail: [email protected]) 2New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 50, Bathurst, New Brunswick, Canada E2A 3Z1 3New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 6000, Fredericton, New Brunswick, Canada E3B 5H1 4Department of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada P3E 2C6 These short course notes provide an overview of published lit- Table 1. List of regional surveys and case studies conducted around erature on the use of scheelite and wolframite as indicator min- the world in which scheelite and/or wolframite in surficial sediments erals for W, Mo, and Au exploration. The use of scheelite and have been used as indicator minerals. wolframite in stream sediments is well documented for mineral Mineral Media Location Source of Information exploration but less so for using glacial sediments (Table 1). scheelite stream sediments Pakistan Asrarullah (1982) wolframite stream sediments Burma ESCAP Scretariat (1982) The Geological Survey of Canada has recently conducted a scheelite, wolframite stream sediments USA Theobald & Thompson (1960) glacial till and stream sediment indicator mineral case study scheelite stream sediments, soil Thailand Silakul (1986) around the Sisson W-Mo deposit in eastern Canada. scheelite stream sediments Greenland Hallenstein et al. (1981) Preliminary indicator mineral results from this ongoing study scheelite stream sediments Spain Fernández-Turiel et al.
    [Show full text]
  • Karacasu Ve Bozdoğan Çapraz Grabenlerinin (Bati Anadolu) Stratigrafik, Sedimantolojik Ve Tektonik Evrimi
    OSMANGAZİ ÜNİVERSİTESİ BİLİMSEL ARAŞTIRMA PROJELERİ KOMİSYONU KARACASU VE BOZDOĞAN ÇAPRAZ GRABENLERİNİN (BATI ANADOLU) STRATİGRAFİK, SEDİMANTOLOJİK VE TEKTONİK EVRİMİ Doç. Dr. Faruk Ocakoğlu Doç. Dr. Kadir Dirik Dr. Ramazan Demirtaş Araş. Gör. Erman Özsayın Jeo. Y. Müh. Sanem Açıkalın FİNAL RAPORU (15 Temmuz 2004-15 Mart 2007) TEŞEKKÜR Bu projenin yürütülmesi sürecinde çeşitli kişi ve kurumlardan önemli destekler aldık. Bozdoğan Belediye başkanı Sayın Tümer Apaydın ikinci arazi sezonu boyunca bizlere Belediye Konuk Evi’nde konaklama olanağı sundu. Karacasu Belediye Başkanı Sayın Emin Mete ve Kuyucak Belediye Başkanı Sayın Ali Ulvi Akoğlu sıcak misafirseverliklerini esirgemediler. TPAO’dan Sayın Hasan Güney kurum yöneticileri ile aramızda dostane bir köprü oldu ve bizi hep güler yüzle karşıladı. Adnan Menderes Üniversitesi Tarih Bölümünden Dr. Günver Güneş 1899 depremine ilişkin belgeleri bizimle cömertlikle paylaştı; ihtiyaç duyduğumuz bazı ek bilgileri Osmanlı arşivlerinden çıkararak bize ulaştırdı. MTA Genel Müdürlüğünden Dr. Gerçek Saraç proje alanından derlenen omurgalı fosillerini tanımlayıp yaşlandırdı. Karacasu Grabeninden alınan örneklerde Dr. Güldemin Öğrünç (Kahramanmaraş Sütçü İmam Üniversitesi) ostrakod faunasını, Prof. Dr. Ayşegül Yıldız (Aksaray Üniversitesi) diyatome faunasını elde edip tanımladılar. Emekleri ölçülemeyecek bütün bu yönetici ve araştırmacılara içten teşekkürlerimizi sunuyoruz. i ÖZET Batı Anadolu Genişleme Bölgesinde yer alan proje alanı kabaca K-G gidişli Karacasu ve Bozdoğan Çapraz Grabenleri ile daha
    [Show full text]
  • Minerals and Mineral Products in Our Bedroom Bed Hematite
    Minerals and Mineral Products in our Bedroom Make-Up Kit Muscovite Bed Talc Hematite: hinges, handles, Mica mattress springs Hematite: for color Chromite: chrome plating Bismuth Radio Barite Copper: wiring Plastic Pail Quartz: clock Mica Gold: connections Cassiterite: solder Toilet Bowl / Tub Closet Feldspar: porcelain Chromite: chrome plating Pyrolusite: coloring Hematite: hinges, handles (steel) Chromite: plumbing fixtures Quartz : mirror on door Copper: tubing Desk Toothpaste Hematite: hinges, handles (steel) Apatite: teeth Chromite: chrome plating Fluorite: toothpaste Mirror Rutile: to color false Hematite: handle, frame teeth yellow Chromite: plating Gold: fillings Gold: plating Cinnabar: fillings Quartz: mirror Towels Table Lamp Sphalerite: dyes Brass (an alloy of copper and Chromite: dyes zinc): base Quartz: bulb Water Pipe/Faucet/Shower bulb Wolframite: lamp filament Brass Copper: wiring Iron Nickel Minerals and Mineral Products in our Bedroom Chrome: stainless steel Bathroom Cleaner Department of Environment and Natural Resources Borax: abrasive, cleaner, and antiseptic MINES AND GEOSCIENCES BUREAU Deodorant Spray Can Cassiterite Chromite Copper Carpet Quartz Sphalerite: dyes Telephone Chromite: dyes Drinking Glasses Copper: wiring Sulfur: foam padding Quartz Chromite: plating Gold: red color Clock Silver: electronics Pentlandite: spring Graphite: batteries Refrigerator Quartz: glass, time keeper Hematite Television Chromite: stainless steel Chromite: plating Computer Galena Wolframite: monitor Wolframite: monitor Copper Copper:
    [Show full text]
  • İzmi̇r History
    İZMİR HISTORY Project Design Strategy Report First Edition, İzmir, 2016 1 Prof. Dr. İlhan Tekeli Prepared for publication by: Dr. H. Gökhan Kutlu Merve Çalışkan, Gizem Akyıldız, Dr. Çağlayan Deniz Kaplan, Alkın Korkmaz First Edition: September, 2016 İzmir Metropolitan Municipality Department of Survey and Project Directorate of Historic Environment and Cultural Properties İzmir History Project Centre 500 Copies Printed By: Dinç Ofset ISBN: 978-975-18-0201-9 2 CONTENTS I.INTRODUCTION 4 II.THESPATIALDIFFERENTIATIONOFTHEPOPULATIONANDTHEECONOMICGROWTH INIZMIR 7 WHATKINDOFASPATIALDIFFERENTIATIONTHEECONOMICGROWTHOFIZMIRSHOWS? 8 THEFORMATIONOFTHEIZMIRCENTERBUSINESSDISTRICT(CBD)ANDTHEFORMATIONDYNAMICSOFTHEIZMIRͲ HISTORYAREAINTHECHANGINGPROCESSINTHECOURSEOFTIME 15 IIIDETERMINATIONOFTHEIZMIRHISTORYPROJECTAREAANDSUBAREAS 34 THEFORMATIONOFTHEIZMIRͲHISTORYPROJECTANDTHELANDUSAGESTATUSESONIT 37 CHANGESTHATWEREEXPERIENCEDDURINGTHEREPUBLICPERIODINTHEIZMIRͲHISTORYPROJECTAREA ECONOMICALACTIVITIESPROFILE 47 DETERMINATIONOFTHESUBAREASOFTHEIZMIRͲHISTORYPROJECT 53 PROCESSOFTHERIFTFORMATIONINTHEIZMIRͲHISTORYPROJECTAREA 66 INFORMATIONABOUTROMANIZMIRINTHEIZMIRͲHISTORYPROJECTAREA 68 IV.STRATEGYPROPOSALOFTHEPRESERVATION/DEVELOPMENTOFIZMIRͲHISTORY PROJECTAREA 70 AIMS 71 STRATEGICALORIENTATION 72 STRATEGIESTHATSHALLBEBENEFITEDINDEVELOPINGTHEIZMIRͲHISTORYPROJECTASPERTHESUBJECTS 74 1.URBANARCHAELOGYANDPRESERVATIONSTRATEGYTHATSHALLBEIMPLEMENTEDINTHEPROJECTREGION 75 2.STRATEGYOFBRINGINGSOMEPLACESINTHEPROJECTAREAINBEINGAPLACEWHICHREALIZESAN“EXPERIENCE” BEYONDBEINGALIFEAREA.
    [Show full text]
  • Metacinnabar Hgs C 2001-2005 Mineral Data Publishing, Version 1
    Metacinnabar HgS c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 43m. Commonly massive; rarely as small (to 1 mm) tetrahedral crystals having rough faces. Twinning: Common on {111}, forming lamellae in polished section. Physical Properties: Fracture: Subconchoidal. Tenacity: Brittle. Hardness = 3 VHN = n.d. D(meas.) = 7.65 D(calc.) = 7.63 Optical Properties: Opaque. Color: Grayish black; in polished section, grayish white. Streak: Black. Luster: Metallic. Pleochroism: Weak, rarely. Anisotropism: Very weak, rarely. R: (400) 28.4, (420) 27.6, (440) 26.8, (460) 26.3, (480) 25.9, (500) 25.6, (520) 25.4, (540) 25.2, (560) 25.1, (580) 25.0, (600) 24.9, (620) 24.9, (640) 24.8, (660) 24.7, (680) 24.7, (700) 24.7 Cell Data: Space Group: F 43m. a = 5.8717(5) Z = 4 X-ray Powder Pattern: Synthetic. 3.378 (100), 2.068 (55), 1.7644 (45), 2.926 (35), 1.3424 (12), 1.6891 (10), 1.3085 (10) Chemistry: (1) (2) (3) (4) Hg 79.73 67.45 81.33 86.22 Zn 4.23 3.10 Cd 11.72 Fe trace 0.2 Se 1.08 6.49 S 14.58 15.63 10.30 13.78 Total 99.62 98.10 98.12 100.00 (1) Guadalc´azar,Mexico; corresponds to (Hg0.85Zn0.14)Σ=0.99(S0.97Se0.03)Σ=1.00. (2) Uland area, Russia; corresponds to (Hg0.69Cd0.21Zn0.10Fe0.01)Σ=1.01S1.00. (3) San Onofre, Mexico; corresponds to Hg1.00(S0.80Se0.20)Σ=1.00.
    [Show full text]
  • A Review on Urbanization, Pollution and Biodiversity in İzmir
    International Journal of Environmental Trends (IJENT) 2019: 3 (1),31-38 ISSN: 2602-4160 Review Article A review on Urbanization, Pollution and Biodiversity in İzmir 1 2 Ece SÖKMEN YILMAZ* , Semih YILMAZ 1 Molkim Industrial Products, Department of Research & Development, İzmir, Turkey 2 Dokuz Eylül University, Maritime Faculty, Department of Marine Engineering, İzmir, Turkey Received 05 November 2018 Abstract Accepted 14 April 2019 Izmir is a town with rich habitats in biodiversity as urbanization is rapidly increasing. In this study, the studies on ecology of Izmir have been compiled and Keywords İzmir important natural areas are mentioned. Urbanization and pollution have also been Ecology noted. Biodiversity Urbanization The purpose of this study is; the bringing together of scientific data on Pollution urbanization, pollution and ecology of Izmir and the constituting a basis for evaluating the factors that threaten the ecological situation and environmental health which are not taken into consideration in the projects planned or the projects to be carried out. International Journal of Environmental Trends, 3 (1), 31-38. DOI: not now possible _________________________ 1 Corresponding Author Email: [email protected] 31 International Journal of Environmental Trends (IJENT) 2019: 3(1), 31-38 INTRODUCTION Although urbanization is an increase in the number of cities and population, it is a process that changes the attitudes and behaviors and social structure of people emerging with some technological, economic, social and political phenomena. As cities include different ethnic groups, cultures, social strata and occupational groups, the relations at individual and group levels differ in cities. The resulting individualization is the source of intergenerational conflict arising from value differences.
    [Show full text]
  • Archaeology and History of Lydia from the Early Lydian Period to Late Antiquity (8Th Century B.C.-6Th Century A.D.)
    Dokuz Eylül University – DEU The Research Center for the Archaeology of Western Anatolia – EKVAM Colloquia Anatolica et Aegaea Congressus internationales Smyrnenses IX Archaeology and history of Lydia from the early Lydian period to late antiquity (8th century B.C.-6th century A.D.). An international symposium May 17-18, 2017 / Izmir, Turkey ABSTRACTS Edited by Ergün Laflı Gülseren Kan Şahin Last Update: 21/04/2017. Izmir, May 2017 Websites: https://independent.academia.edu/TheLydiaSymposium https://www.researchgate.net/profile/The_Lydia_Symposium 1 This symposium has been dedicated to Roberto Gusmani (1935-2009) and Peter Herrmann (1927-2002) due to their pioneering works on the archaeology and history of ancient Lydia. Fig. 1: Map of Lydia and neighbouring areas in western Asia Minor (S. Patacı, 2017). 2 Table of contents Ergün Laflı, An introduction to Lydian studies: Editorial remarks to the abstract booklet of the Lydia Symposium....................................................................................................................................................8-9. Nihal Akıllı, Protohistorical excavations at Hastane Höyük in Akhisar………………………………10. Sedat Akkurnaz, New examples of Archaic architectural terracottas from Lydia………………………..11. Gülseren Alkış Yazıcı, Some remarks on the ancient religions of Lydia……………………………….12. Elif Alten, Revolt of Achaeus against Antiochus III the Great and the siege of Sardis, based on classical textual, epigraphic and numismatic evidence………………………………………………………………....13. Gaetano Arena, Heleis: A chief doctor in Roman Lydia…….……………………………………....14. Ilias N. Arnaoutoglou, Κοινὸν, συμβίωσις: Associations in Hellenistic and Roman Lydia……….……..15. Eirini Artemi, The role of Ephesus in the late antiquity from the period of Diocletian to A.D. 449, the “Robber Synod”.……………………………………………………………………….………...16. Natalia S. Astashova, Anatolian pottery from Panticapaeum…………………………………….17-18. Ayşegül Aykurt, Minoan presence in western Anatolia……………………………………………...19.
    [Show full text]
  • Uşak İli Buğday (Triticum Aestivum L.) Ekim Alanlarında Sorun Olan Yabancı Ot Türlerinin, Yaygınlık Ve Yoğunluklarının Belirlenmesi¥
    Türk Tarım ve Doğa Bilimleri Dergisi 7(2): 349–367, 2020 https://doi.org/10.30910/turkjans.725793 TÜRK TURKISH TARIM ve DOĞA BİLİMLERİ JOURNAL of AGRICULTURAL DERGİSİ and NATURAL SCIENCES www.dergipark.gov.tr/turkjans Araştırma Makalesi Uşak İli Buğday (Triticum aestivum L.) Ekim Alanlarında Sorun Olan Yabancı Ot Türlerinin, Yaygınlık ve Yoğunluklarının Belirlenmesi¥ Derya KÖKTAŞ1, Derya ÖĞÜT YAVUZ2* 1Uşak Üniversitesi, Fen Bilimleri Enstitüsü, Tarım Bilimleri, Uşak 2Uşak Üniversitesi, Ziraat ve Doğa Bilimleri Fakültesi, Bitki Koruma, Uşak *Sorumlu yazar: [email protected] Geliş Tarihi: 27.08.2019 Düzeltme Geliş Tarihi: 08.12.2019 Kabul Tarihi: 04.02.2020 Özet Yabancı otlar % 48-52 oranlarında kayıpla diğer biyotik faktörlerden ön plana çıkmakta, rekabet ve salgıladığı allelopatik maddelerle buğdayda ürün kalitesinin düşmesine ve verim kaybına neden olmaktadır. Bu nedenle Uşak ili buğday alanlarında yürütülen bu çalışmada yabancı otların tür ve yoğunluklarının belirlenmesi, mücadele çalışmalarına kaynak oluşturması açısından önem arz etmektedir. Çalışma, Uşak ilini temsil edecek şekilde altı ilçede (Merkez, Banaz, Eşme, Karahallı, Ulubey ve Sivaslı) toplam 115 tarlada, mücadele yapılıp yapılmaması gözetilmeksizin buğday ekim alanları gezilerek yabancı otların tür, yaygınlık ve yoğunluklarının belirlenmesi amacıyla yürütülmüştür. Yapılan çalışma sonucunda Uşak ili buğday alanlarında 24 familyaya ait 11’i cins, 65’i tür ve tür altı takson düzeyinde toplam 76 takson tespit edilmiştir. İl bazında elde edilen sonuçlara göre yabancı
    [Show full text]
  • A Survey of the Gemstone Resources of China
    A SURVEY OF THE GEMSTONE RESOURCES OF CHINA By Peter C. Keller and Wang Fuquan The People's Republic of China has recently hina has historically been a land of great mystery, placed a high priority on identifying and C with natural resources and cultural treasures that, developing its gemstone resources. Initial until recently, were almost entirely hidden from the out- exploration by teams of geologists side world. From the point of view of the geologist and throughout China has identified many gemologist, one could only look at known geological maps deposits with significant potential, of this huge country and speculate on the potential impact including amher, cinnabar, garnets, blue sapphires, and diamonds. Small amounts of China would have on the world's gem markets if its gem ruby have' qlso been found. Major deposits resources were ever developed to their full potential. of nephriteyade as well as large numbers of During the past few years, the government of the Peo- gem-bearing pegmatite dilces have been ple's Republic of China (P.R.C.)has opened its doors to the identified.Significant deposits of peridot outside world in a quest for information and a desire for are crirrently being exploited from Hebei scientific and cultural cooperation. It was in this spirit of Province. Lastly, turqrloise rivaling the cooperation that a week-long series of lectures on gem- finest Persian material has been found in stones and their origins was presented by the senior author large quantities in Hubei and Shaanxi and a colleague to over 100 geologists from all over China Provinces.
    [Show full text]
  • 2018-2022 Aydın Tarım Vizyonu.Pdf
    AYDIN TARIM VİZYONU 2018-2022 Bakanlığımız stratejik planında yer alan 7 alan, 7 amaç doğrultusunda Bakanlığımızın ülke çapında belirlemiş olduğu hedeflere ilave olarak, yerelde 51 hedef ile; sürdürülebilir tarım için bitki desenimiz, hayvan varlığımız ve su ürünleri kaynaklarımıza göre ilimizde kırsal yaşam standartlarının yükseltilmesini ve sektörel sorunların çözülmesini Bakanlığımızın Ar-Ge çalışmalarıyla destekleyerek vizyoner yaklaşımla ilimizin strateji belgesini oluşturduk. 1 I.BÖLÜM MEVCUT DURUM 2 AYDIN İLİ ARAZİ VARLIĞI % 11.54 % 3.13 Tarım dışı Çayır Arazi Kullanım Şekli Alan (ha) % + Göl Mera Bataklık Kültür Arazisi 364.943 44,97 % 44.97 Orman 327.606 40,37 %40.37 Kültür Arazisi Tarım Dışı + Göl-Bataklık Orman 93.632 11,54 Araziler Çayır Mera Arazisi 25.419 3,13 TOPLAM 811.600 100,00 3 HAYVAN VARLIĞI Deve;490 Kedi-Köpek; 16.580 Manda; 183 Tek Tırnaklı; 9.908 Sığır; Arılı Kovan 444.960 274.826 Koyun 257.162 Keçi; 103.962 İlimizde bulunan Büyükbaş hayvanların saf kültür ırklarının yüzdesi % 76 Türkiye ortalaması % 44 dür. 4 ÖNEMLİ HAYVANSAL ÜRÜNLERİMİZ (2019) ÜRETİMDEKİ PAYIMIZ İLİMİZİN TÜRKİYE ÜRÜNLER AYDIN İLİ ÜRETİMİ (%) SIRALAMASI YAVRU BALIK 145 milyon (adet) 30 2 BAL 4.227 ton 3.7 5 SÜT 546.164 ton 2.3 6 BÜYÜKBAŞ HAYVAN 22.950 ton 2.5 8 48 adet 928.725 ton kapasiteli Süt Ürünleri İşletmemizde; Süt üretimimizin % 42,23’ü 230.680 ton’u süt ürünlerine işlenmektedir. 5 İHRACATIMIZ İHRAÇ EDİLEN ÜRÜNLER 2018 (Ton) 2019 (Ton) KURU ÜRÜNLER 51.901 59.935 TAZE MEYVE SEBZE 14.016 11.654 ZEYTİN 22.686 26.871 ZEYTİNYAĞI 205 127 BİTKİSEL
    [Show full text]
  • A Deposit Model for Mississippi Valley-Type Lead-Zinc Ores
    A Deposit Model for Mississippi Valley-Type Lead-Zinc Ores Chapter A of Mineral Deposit Models for Resource Assessment 2 cm Sample of spheroidal sphalerite with dendritic sphalerite, galena, and iron sulfides (pyrite plus marcasite) from the Pomorzany mine. Note the “up direction” is indicated by “snow-on-the-roof” texture of galena and Scientificsphalerite Investigations alnong colloform Report layers of2010–5070–A light-colored spahlerite. Hydrothermal sulfide clasts in the left center of the sample are encrusted by sphalerire and iron sulfides. Size of sample is 20x13 cm. Photo by David Leach. U.S. Department of the Interior U.S. Geological Survey COVER: Sample of spheroidal sphalerite with dendritic sphalerite, galena, and iron sulfides (pyrite plus mar- casite) from Pomorzany mine. Note the “up direction” is indicated by “snow-on-the-roof” texture of galena and sphalerite along colloform layers of light-colored sphalerite. Hydrothermal sulfide clasts in the left center of the sample are encrusted by sphalerite and iron sulfides. Size of sample is 20x13 centimeters. (Photograph by David L. Leach, U.S. Geological Survey.) A Deposit Model for Mississippi Valley- Type Lead-Zinc Ores By David L. Leach, Ryan D. Taylor, David L. Fey, Sharon F. Diehl, and Richard W. Saltus Chapter A of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–A U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S.
    [Show full text]