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30 th International Conference on “Ore Potential of Alkaline, Kimberlite and Carbonatite Magmatism” 29 September - 02 October 2014 Antalya - TURKEY ABSTRACT BOOK Editors & ABSTRACT BOOK ABSTRACT Assoc. Prof. Dr. Nurdane ILBEYLI Prof. Dr. M. Gurhan YALCIN Ore Potential of Alkaline, Kimberlite & Carbonatite Magmatism 30th International Conference on “Ore Potential of Alkaline, Kimberlite and Carbonatite Magmatism” ABSTRACTS BOOK 29 September - 02 October 2014 Antalya - TURKEY Editors Assoc.Prof.Dr. Nurdane ILBEYLI and Prof.Dr. M. Gurhan YALCIN i 550.4 30th International Conference on “Ore Potential of Alkaline, Kimberlite and Carbonatite Magmatism” Abstract Book Akdeniz University-Antalya / UCTEA Chamber of Turkish Geological Engineers-Ankara / 2014 258 pages Figure, Table Alkaline, Kimberlite, Carbonatite, Magmatism, Ore Potential, Diamond ISBN: Press: All rights reserved. Citing the source can be quoted. The authors are responsible for the contents of the abstracts. ii HONORARY PRESIDENT President – Akdeniz University, TURKEY Prof.Dr. Israfil KURTCEPHE ORGANIZING BOARD Akdeniz University, TURKEY Russian Academy of Sciences, RUSSIA Ukraine Academy of Sciences, UKRAINE UCTEA Chember of Turkish Geological Engineers, TURKEY ORGANIZING COMMITTEE Chairmen of the Organizing Committee Assoc.Prof.Dr. Nurdane ILBEYLI Prof.Dr. M. Gurhan YALCIN Co-Chairman of the Organizing Committee Academician RAS Lia N. KOGARKO Organizing & Social Secretariat Lecturer Fusun YALCIN Logistic Secretariat Assist.Prof.Dr. Yasemin LEVENTELI Assistant Secretariat Res.Asst. Ebru PAKSU Treasurer Assoc.Prof.Dr. Burcu DEMIREL UTKU Logo & Flyer Design Assist.Prof.Dr. Mehmet DEMIRBILEK Web Design Res.Asst. Halil BOLUK Members Prof.Dr. Eugenii M. SHEREMET Academician RAS Igor D. RYABCHIKOV Prof. Dr. David R. LENTZ Natalia V. SOROKHTINA Vera N. ERMOLAEVA Victor A. ZAITSEV iii SCIENTIFIC COMMITTEE Prof.Dr. Ercan ALDANMAZ Kocaeli University Prof.Dr. Mesut ANIL Cukurova University Assoc.Prof.Dr. Faruk AYDIN Karadeniz Technical University Assist.Prof.Dr. Metin BAGCI Afyon Kocatepe University Prof.Dr. A. Feyzi BINGOL Firat University Assoc.Prof.Dr. Emin CIFTCI Istanbul Technical University Prof.Dr. Ibrahim COPUROGLU Nigde University Vera N. ERMOLAEVA GEOKHI RAS Assoc.Prof.Dr. Murat HATIPOGLU Dokuz Eylul University Prof.Dr. Cahit HELVACI Dokuz Eylul University Prof.Dr. Yusuf Kagan KADIOGLU Ankara University Assoc.Prof.Dr. Leyla KALENDER Firat University Prof.Dr. Muazzez CELIK KARAKAYA Selcuk University Assoc.Prof.Dr. Abdullah KAYGUSUZ Gumushane University Prof.Dr. Yasar KIBICI Dumlupinar University Dr. Serpil KILIC Akdeniz University Academician RAS Lia N. KOGARKO Russian Academy of Sciences Prof. Dr. David R. LENTZ University of New Brunswick Prof.Dr. Halim MUTLU Ankara University Prof.Dr. Ayten OZTUFEKCI ONAL Tunceli University Prof.Dr. Yuksel ORGUN Istanbul Technical University Prof.Dr. Yahya OZPINAR Pamukkale University Prof.Dr. Osman PARLAK Cukurova University Academician RAS Igor D. RYABCHIKOV IGEM RAS Prof.Dr. Burhan SADIKLAR Karadeniz Technical University Prof.Dr. Ahmet SAGIROGLU Firat University Prof.Dr. Sabah YILMAZ SAHIN Istanbul University Assoc.Prof.Dr. Ender SARIFAKIOGLU Gen. Dir. of Mineral Res. and Exp. Prof.Dr. Kadir SARIIZ Osmangazi University Prof.Dr. Mehmet SENER Nigde University Prof.Dr. Eugenii M. SHEREMET Ukrainian Academy of Sciences Natalia V. SOROKHTINA GEOKHI RAS Prof.Dr. Abidin TEMEL Hacettepe University Prof.Dr. Taner UNLU Ankara University Assist.Prof.Dr. Yusuf URAS Sutcu Imam University Assoc.Prof.Dr. Ahmet YILDIZ Afyon Kocatepe University Victor A. ZAITSEV GEOKHI RAS PREFACE In recent years, alkaline rocks have started to attract intensive attention in both academ- ic and practical fields. These rocks are distinguished mostly by the abundance of alka- line minerals they contain rather than their other components. They generally represent magmatic rocks which contain sodium pyroxene, sodium amphibole or feldspathoid. Alkaline magmatic rocks are produced from magmas originating from the partial fu- sion of the upper mantle peridotites in different types and degrees. Their role in creating rich mineral deposits increased their significance. Diamond deposits in kimberlite pipes are one of the most important examples. Carbonatites are the latest products of differ- entiation processes of alkaline mafic (nepheline) or ultramafic (kimberlite) magmas and they may create essential deposits (Nb, Ta, Th, Cu and other metals in addition to nonmetallic minerals such as apatite, barite, fluorite, strontianite, phlogopite, REEs, vermiculite and baddeleyite). The 30th international conference of “Ore Potential of Alkaline, Kimberlite and Carbon- atite Magmatism”, previous ones of which were held in different cities in Russia and Ukraine by Vernadsky Institute of Geochemistry and Analytical Chemistry every year since 1983, will be held in Antalya, Turkey this year. 22 country representatives from Algeria, Australia, Azerbaijan, Belarus, Brazil, Cana- da, China, Congo, Egypt, Georgia, Germany, Hungary, Iran, Kuwait, Poland, Russia, South Korea, Switzerland, Turkey, Ukraine, UK and USA are expected to participate in the conference. There are approximately 115 statements and posters sent from the participant countries. 42 of these works are verbal statements and the rest are poster presentations. The number of guests and participants are approximately 150. The active participation shows the success rate of the conference. On the first three days of the conference, which will be held on 29 September – 02 Oc- tober 2014, scientific presentations and posters will be presented and on the fourth day, there will be a technical trip to Antalya - Tekirova area. This book contains abstracts and/or indicative abstracts of the statements and posters which will be presented in 30th International Conference on “Ore Potential of Alkaline, Kimberlite and Carbonatite Magmatism” conference which is held by Akdeniz University, Faculty of Engineer- ing, Department of Geological Engineering and supported by Chamber of Geologi- cal Engineers of Turkey. Talks and posters to be presented in the conference involves “genesis of alkaline magmatism; genesis of kimberlites and other ultrapotassic rocks; experimental data for petrogenesis of alkaline rocks; geochemistry, petrology and ore potential of alkaline-carbonatitic, mafic and ultramafic rocks and granitoids; mineral- ogy, crystalochemistry of alkaline rocks and carbonatites and others” and detailed in- formation about the subjects can be found in this book. We wish that this abstract book contributes to international science community. Assoc.Prof.Dr. Nurdane ILBEYLI Prof.Dr. M. Gurhan YALCIN Chairman of the Organizing Committee Chairman of the Organizing Committee TABLE OF CONTENTS GEOCHEMISTRY OF OUED AMIZOUR IGNEOUS ROCKS (BEJAIA, EASTERN ALGERIA) Abderrahmane H., Benali H. ............................................................................... 1 MAFIC layered COMPLExES coeval to FELSIC COMPLExES IN THE LATEA metacraton (HOGGAR ALGERIA):AN ExAMPLE OF ALLIOUM-IN Amertek-OUKCEM COMPLExES Implications FOR POST-COLLISIONAL IGNEOUS EPISODES IN THE PANAFRICAN OROGEN Azzouni-Sekkal A., Ikhlef-Debabha F., Aïdrous-Belhocine K., Bonin B., Liégeois J. P. ........................................................................................... 2 GEOCHEMICAL Features OF ALKALINE Magmatism - Related FLOURITE DEPOSITS OF TURKEY Altuncu S., Oztürk H. ............................................................................................ 4 Granitoids OF DIFFERENT GEOCHEMICAL TYPES OF BAIKAL AREA (RUSSIA), THEIR ORIGIN AND RARE Metal POTENTIAL Antipin V.S., Gorlacheva N.V. ............................................................................... 6 PETROGRAPHICAL AND GEOCHEMICAL Properties OF THE MAFIC (GABBROIC) ROCKS, (TURKEY, KINIK - Kütahya) Arat I., Yanık G., Kibici Y., Ilbeyli N., Ozkul C. ................................................ 9 DYKES IN THE northeastern FENNOSCANDIAN SHIELD: A KEY FOR PALEOZOIC MAGMAS EMPLACEMENT AND estimation OF primary MANTLE melts COMPOSITION Arzamastsev A. A. .................................................................................................. 10 Behavior OF ALKALI, ALKALI-earth AND RARE-earth ELEMENTS OF trachybasalt-TRACHYDOLERITE AND TEPHRITE-TESCHENITE COMPLExES OF Khojavend TROUGH Babayeva G.J., Mammadov M.N., Gasanguliyeva M.Y. .................................... 12 RARE OCCURRENCE PLATINUM GROUP IN ESFANDAGH OPHIOLITE COMPLEx (SW OF KERMAN , IRAN) Bagheriyan S........................................................................................................... 14 A SELECTIVE AND EFFICIENT METHOD FOR THE ADSORPTION AND Separation OF ARSENIC Metal ION FROM WASTE Waters BY MAGNETIC SOLID-PHASE ExTRACTION WITH MODIFIED MAGNETIC Nanoparticles Bagheriyan S........................................................................................................... 15 SINGULAR SYNERGISTIC EFFECTS OF Expanded nanoclay ON FLAME retardant ABS/SB2O3/BROMINE HYBRID NANOCOMPOSITES Bagheriyan S........................................................................................................... 16 Mineralization OF qUADRANGLE OF ALIGODARZ ARIA (WEST OF IRAN) USING GEOMAGNETISM data OF satellite IMAGES Bagheriyan S........................................................................................................... 18 RARE OCCURRENCE platinum GROUP IN Esfandagh OPHIOLITE COMPLEx (SW OF KERMAN , IRAN) Bagheriyan S..........................................................................................................
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  • TUGTUPITE: a GEMSTONE from GREENLAND by Aage Jensen and Ole V

    TUGTUPITE: a GEMSTONE from GREENLAND by Aage Jensen and Ole V

    TUGTUPITE: A GEMSTONE FROM GREENLAND By Aage Jensen and Ole V. Petersen The red variety of the mineral tugtupite, a rare is derived from the locality where the mineral silicate closely related to sodalite, has been used as was first found. In 1965, the Commission on New a gemstone since 1965. This article presents the Minerals and Mineral Names of the International history of the mineral and details of its mineralogy Mineralogical Association approved both the and gemology. A recently discovered light blue mineral and the name. variety of tugtupite is also described. Thus far, Dan0 (1966) described the crystal structure of tugiupite has been found in only two localities: (1) tugtupite. A detailed description of the crystal Lovozero, Kola Peninsula, U.S.S.R., where it occurs as very small1 grains; and (2) Ilimaussaq, South habit, the pseudocubic penetration trillings, and Greenland, where it has been located at several the numerous localities where tugtupite had been places within the Ilimaussaq intrusion. Gem-quality found from the time that it was first traced at tugtupite has come almost exclusively from one Tugtup agtalzorfia until 1971 (including the only occurrence, a set of hydrothermal albite veins from one that has produced gem material of any sig- the Kvanefjeld plateau in the northwestern corner of nificance) was presented by S0rensen et al. (1971). the Ilimaussaq intrusion. Another type of twin, pseudotrigonal contact trillings, was subsequently described by Petersen (19781. The tugtupite from the type locality was The mineral that is now known as tugtupite was described as white, but Sflrensen (1960)mentions discovered in 1957 by Professor H.
  • Identification Tables for Common Minerals in Thin Section

    Identification Tables for Common Minerals in Thin Section

    Identification Tables for Common Minerals in Thin Section These tables provide a concise summary of the properties of a range of common minerals. Within the tables, minerals are arranged by colour so as to help with identification. If a mineral commonly has a range of colours, it will appear once for each colour. To identify an unknown mineral, start by answering the following questions: (1) What colour is the mineral? (2) What is the relief of the mineral? (3) Do you think you are looking at an igneous, metamorphic or sedimentary rock? Go to the chart, and scan the properties. Within each colour group, minerals are arranged in order of increasing refractive index (which more or less corresponds to relief). This should at once limit you to only a few minerals. By looking at the chart, see which properties might help you distinguish between the possibilities. Then, look at the mineral again, and check these further details. Notes: (i) Name: names listed here may be strict mineral names (e.g., andalusite), or group names (e.g., chlorite), or distinctive variety names (e.g., titanian augite). These tables contain a personal selection of some of the more common minerals. Remember that there are nearly 4000 minerals, although 95% of these are rare or very rare. The minerals in here probably make up 95% of medium and coarse-grained rocks in the crust. (ii) IMS: this gives a simple assessment of whether the mineral is common in igneous (I), metamorphic (M) or sedimentary (S) rocks. These are not infallible guides - in particular many igneous and metamorphic minerals can occur occasionally in sediments.