Bulletin of the Mineral Research and Exploration

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Bulletin of the Mineral Research and Exploration Bull. Min. Res. Exp. (2017) 154:135-156 154 BULLETIN OF THE MINERAL RESEARCH AND EXPLORATION Foreign Edition 2017 154 ISSN: 0026-4563 BULLETIN OF THE MINERAL RESEARCH AND EXPLORATION RESEARCH THE MINERAL BULLETIN OF CONTENTS One of the Main Neotectonic Structures in the NW Central Anatolia: Beypazarı Blind Thrust Zone and Related Fault- Propagation Folds Bulletin of the Mineral .........................................................................................................................Gürol SEYİTOĞLU, Korhan ESAT and Bülent KAYPAK 1 Structural Features of the Niğde Massif in the Çamardı (Niğde) District ..............................................................................................................................................Ramazan DEMİRCİOĞLU and Yaşar EREN 15 Stratigraphy and Structure of the Southeastern Part of Piramagroon Anticline, Sulaimani Area, Northeast Iraq .......................................................................................................................................Kamal Haji KARIM and Polla Azad KHANAQA 27 An Approach to Coast Edge Line at the Eastern Antalya Marginal-Marine Sea Sides ................................................................................................................Muhittin GÖRMÜŞ, Levent BAŞAYİĞİT and Ahmet UYSAL 41 Grain Size, Total Heavy Mineral and Element Distribution and Control Factors Of Current Sediments on the Floor of Hisarönü and Datça Bays .............................................................................................Barbaros ŞİMŞEK, Mustafa ERGİN, Murat EVREN, Özgür TÜRKMEN, 59 Serkan PALAS, Hakan PEHLİVAN, Bahri Serkan AYDEMİR and Füsun ÖCAL Maastrichtian-Selandian Planktonic Foraminifera Biostratigraphy and Palaeoecological Interpretation of Akveren Formation in Bartin Area (Western Black Sea, Turkey) ....................................................................................................................................................................................... Caner KAYA ÖZER 83 Sedimentology, Mineralogy and Origin of the First Discover Magnesite-Dolomite Belt in Ma’rib District, SW Arabian Peninsula .......................................................................................................................................................... Sa’ad Zeki A.kader AL-MASHAIKIE 109 Sodium Sulfate (Glauberite-Bloedite) - Halite Association in the Tertiary (Upper Miosene - Pliocene) Katrandedetepe Formation, Ereğli-Bor Basin, Turkey Research and Exploration ............................................................... Gökhan KADINKIZ, Memet PEKGÖZ, Mustafa KARAKAŞ and Abdurrahman MURAT 135 Permeability of Savcıbey Dam (Bilecik) Axis Location and Design of Grout Curtain .....................................................................................................................................Mustafa Can CANOĞLU and Bedri KURTULUŞ 157 The Importance of Amount of Settlement in Determining the Bearing Capacity of Soils ..................................................................................................................Selçuk ALEMDAĞ, Aslıhan CİNOĞLU and Elif GACENER 169 Investigation of Güllük (Muğla) Wetland Using Stable Isotopes (δ18O, δD) ............................................................................................................................................................................................ Melis A. SOMAY 181 Assessment of Groundwater Metal-Metalloid Content Using Geostatistical Methods in Karabağlar Polje (Muğla, Turkey) ...........................................................................................................................Bedri KURTULUŞ , Çağdaş SAĞIR and Özgür AVŞAR 193 An Investigation on Single-Particle Impact Breakage Functions of a Gold Ore by Drop-Weight Technique ............................................................................................................................................................................................ Ömürden GENÇ 207 The Reaction of Physical Transformation of the Gravity Data And Linearity Dilemma ................................................................................................................................................................................................. Ertan TOKER Phone : +90 (312) 201 10 00 2017 215 Fax : +90 (312) 287 91 88 Response to the “Reaction of the Physical Transformation of the Gravity Data and Linearity Dilemma” ..................................................................................................................................................................................................... Uğur AKIN 219 http://bulletin.mta.gov.tr Adress : MTA 06520 - Ankara - TURKEY Bulletin of the Mineral Research and Exploration Notes to the Authors ............................................................................................... 221 SODIUM SULFATE (GLAUBERITE-BLOEDITE) - HALITE ASSOCIATION in the TERTIARY (UPPER MIOSENE-PLIOCENE) KATRANDEDETEPE FORMATION, EREĞLİ-BOR BASIN, TURKEY Gökhan KADINKIZa*, Memet PEKGÖZa, Mustafa KARAKAŞb and Abdurrahman MURATc aGeneral Directorate of Mineral Research and Exploration (MTA), Department of Mineral Research and Exploration, Ankara, Turkey bGeneral Directorate of Mineral Research and Exploration (MTA), Konya Regional Directorate, Konya, Turkey cTurkish Coal Enterprises, Ankara, Turkey Research Article Keywords: ABSTRACT Ereğli-Bor Basin, This study covers the investigations related to the glauberite-halite minerals detected in Neogene deposits of the Ereğli- Katrandedetepe Formation, Bor Basin in the Central Anatolia. The basin consists of Paleozoic basement rocks, the unconformably overlying halite, glauberite, bloedite. Paleocene-Eocene-Oligocene marine sedimentary and volcano-sedimentary rocks, and the Lower Miocene-Pliocene lake deposits at the top which unconformably overlie all underlying layers. In the study, core drillings related to the determination of geological characteristics and investigation of the mineral potential of buried salt deposits were carried out in the Ereğli-Bor basin. As a result of drillings carried out, glauberite-bloedite, halite and bituminous shale horizons, which possess significant thickness and grade values, were cut for the first time in the Konya-Ereğli-Bor basin. Glauberite minerals were observed in three different structures as; 1- the Glauberite Mineral intercalated with High Graded, Bedded Clays, 2- the Glauberite Mineral with Disseminated Rosette Type in Low Graded Clays and 3- the Prismatic High Graded Glauberite Mineral intercalated with Halites. Bloedite minerals are mostly observed with halite. Received: 08.05.2016 It was detected that the economical evaporitic formations in the Konya-Ereğli-Bor Basin had occurred within the Upper Accepted: 23.06.2016 Miocene-Pliocene Katrandedetepe formation which represents the playa-lake environment. 1. Introduction authors mentioned about 20 billion tons of apparent operable pure anhydrite reservoirs in their studies, The purpose of the study is to explore probable which they had carried out to explore evaporitic burial type evaporitic industrial raw material deposits salt, and related sedimentary sulfide deposits in in the Ereğli-Bor Basin and their affordability. the Ereğli-Bor Basin. The investigators also stated that the hydrothermal fluids, which were the final As it is known, evaporitic basins are natural products of the Upper Eocene island arc volcanism chemical deposits and accepted as the source of various during the formation of anhydrite, provided ions that industrial raw material. The Ereğli-Bor Basin is an would supply salts to the depositional environment, important basin when the characteristics of geological and also the cherts located within these anhydrites and depositional environments are taken into had supported this formation. Later, Murat (1996) consideration in terms of chemical sedimentary raw materials (sodium sulfate, halite, gypsum/anhydrite studied the distribution and the economic potential etc.) and other raw materials (lignite, bituminous shale of celestines located in the limestone lenses among etc.). Therefore; several investigations have been Ereğli-Ulukışla Tertiary units. carried out in the region. Other studies have also been carried out in Turkey Studies, which are generally related to the in similar Tertiary basins. Helvacı et al. (1987), stated investigation of the regional geology in the basin, were that the Neogene deposits in the Western Anatolia carried out by Türkünal, 1972; Oktay, 1982; Yoldaş, consisted of significant lignite, bituminous shale, 1973; Demirtaşlı et al., 1986; Ayhan et al., 1986 and uranium and borate deposits. Altay (2010) studied the Ercan et al., 1992. The preliminary study in this region mineralogical-geochemical features of the Neogene on evaporites belongs to Özgüner et al. (1989). The sedimentary units in Bor-Ulukışla Basin. Önal et * Corresponding author: Sa’ad Zeki A.kader Al-Mashaikie, [email protected] http://dx.doi.org/10.19111/bulletinofmre.298685 135 Bull. Min. Res. Exp. (2017) 154:135-156 al. (2004) specified that the trona occurrences were cuts excavated for various purposes and drilling wells intercalated with bituminous shale, mudstone and tuffs were studied on the site. Oil, irrigation and potable inside the Terzioğlu Member of the Gürün formation, water drillings made by TPAO, DSI and private in the article of “The Geology and the Trona Potential people were correlated
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