Data Set of World Phosphate Mines, Deposits, and Occurrences—Part B
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Kosnarite Kzr2(PO4)3 C 2001-2005 Mineral Data Publishing, Version 1
Kosnarite KZr2(PO4)3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal, pseudocubic. Point Group: 32/m. As rhombohedral pseudocubic crystals, to 0.9 mm, with {1012} and tiny {0001}. Physical Properties: Cleavage: Perfect on {1012}. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 4.5 D(meas.) = 3.194(2) D(calc.) = 3.206 Optical Properties: Transparent to translucent. Color: Pale blue to blue-green, bluish gray, nearly colorless. Streak: White. Luster: Vitreous. Optical Class: Uniaxial (+). ω = 1.656(2) = 1.682(2) Cell Data: Space Group: R3c. a = 8.687(2) c = 23.877(7) Z = 6 X-ray Powder Pattern: Mt. Mica, Maine, USA. 4.329 (100), 3.806 (90), 2.928 (90), 6.41 (50), 4.679 (50), 2.502 (50), 1.903 (45) Chemistry: (1) (2) (3) P2O5 43.3 42.2 42.04 ZrO2 44.5 47.9 48.66 HfO2 0.5 0.9 FeO 0.2 < 0.1 MnO 1.0 < 0.1 Na2O 1.4 < 0.1 K2O 8.7 9.25 9.30 Rb2O 0.25 0.2 F 0.20 0.2 −O=F2 0.08 0.08 Total 99.97 100.57 100.00 (1) Mt. Mica, Maine, USA; by electron microprobe, total Fe as FeO, total Mn as MnO; corresponds to (K0.93Na0.08Rb0.01)Σ=1.02(Zr1.81Na0.15Mn0.07Fe0.01Hf0.01)Σ=2.05 [P1.02(O3.98F0.02)Σ=4.00]3. (2) Black Mountain, Maine, USA; by electron microprobe, total Fe as FeO, total Mn as MnO; corresponds to (K0.99Rb0.01)Σ=1.00(Zr1.96Hf0.02)Σ=1.98 [P1.00(O3.98F0.02)Σ=4.00]3. -
Geology of the Hugo Pegmatite Keystone, South Dakota
Geology of the Hugo Pegmatite Keystone, South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-B Geology of the Hugo Pegmatite Keystone, South Dakota By J. J. NORTON, L. R. PAGE, and D. A. BROBST PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-P A detailed structural and petrologic study of a pegmatite containing seven zones and two replacement bodies UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Abstract.. _ ________________________________________ 49 Mineral distribution and paragenesis of the entire Introduction. ______________________________________ 49 pegmatite_ _ ______________________-___---------_ 96 General geology. ___________________________________ 52 Comparison of the zonal sequence with that in other Metamorphic rocks_ ____________________________ 52 pegmatites. ______________________________________ 97 Roy and Monte Carlo pegmatites.- _ __---__-______ 53 Replacement features-______________________________ 100 Structure __________________________________________ 53 Review of the evidence for replacement in pegma Pegmatite units ____________________________________ 53 tites __ _____________________________________ 100 Zone 1 : Albite-quartz-musco vite pegmatite ________ 56 Replacement in the Hugo pegmatite.____-_____-_- 102 -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
Program and Abstracts
The Atlantic Geoscience Society (AGS) La Société Géoscientifique de l’Atlantique 45th Colloquium and Annual Meeting Special Sessions: • Special Session: In Memory of Dr. Trevor MacHattie (1974 - 2018) • Paleontology and Sedimentology in Atlantic Canada: In Memory of Dr. Ron Pickerill (1947 – 2018) • Current Research in Carboniferous Geology in the Atlantic Provinces • Minerals, metals, melts, and fluids associated with granitoid rocks: new insights from fundamental studies into the genesis, melt fertility, and ore-forming processes • Earth Science Outreach in the Maritime Provinces • Geohazards: Recent and Historical General Sessions: Current Research in the Atlantic Provinces February 7-9, 2019 Fredericton Inn, Fredericton, New Brunswick PROGRAM WITH ABSTRACTS We gratefully acknowledge sponsorship from the following companies and organizations: Department of Energy and Resource Development Geological Surveys Branch Department of Energy and Mines Department of Energy and Mines Geological Surveys Division Petroleum Resources Division Welcome to the 45th Colloquium and Annual Meeting of the Atlantic Geoscience Society in Fredericton, New Brunswick. This is a familiar place for AGS, having been a host several times over the years. We hope you will find something to interest you and generate discussion with old friends and new. AGS members are clearly pushing the boundaries of geoscience in all its branches! Be sure to take in the science on the posters and the displays from sponsors, and don’t miss the after-banquet jam and open mike on Saturday night. For social media types, please consider sharing updates on Facebook and Twitter (details in the program). We hope you will be able to use the weekend to renew old acquaintances, make new ones, and further the aims of your Atlantic Geoscience Society. -
Modern Laments in Northwestern Greece, Their Importance in Social and Musical Life and the “Making” of Oral Tradition
Karadeniz Technical University State Conservatory © 2017 Volume 1 Issue 1 December 2017 Research Article Musicologist 2017. 1 (1): 95-140 DOI: 10.33906/musicologist.373186 ATHENA KATSANEVAKI University of Macedonia, Thessaloniki, Greece [email protected] orcid.org/0000-0003-4938-4634 Modern Laments in Northwestern Greece, Their Importance in Social and Musical Life and the “Making” of Oral Tradition ABSTRACT Having as a starting point a typical phrase -“all our songs once were KEYWORDS laments”- repeated to the researcher during fieldwork, this study aims Lament practices to explore the multiple ways in which lament practices become part of other musical practices in community life or change their Death rituals functionalities and how they contribute to music making. Though the Moiroloi meaning of this typical phrase seems to be inexplicable, nonetheless as Musical speech a general feeling it is shared by most of the people in the field. Starting from the Epirot instrumental ‘moiroloi’, extensive field research Lament-song reveals that many vocal practices considered by former researchers to Symbolic meaning be imitations of instrumental musical practices, are in fact, definite lament vocal practices-cries, embodied and reformed in different ways Collective memory in other musical contexts and serving in this way different social purposes. Furthermore, multiple functionalities of lament practices in social life reveal their transformations into songs and the ways they contribute to music making in oral tradition while at the same time confirming the flexibility of the border between lament and song established by previous researchers. Received: November 17, 2017; Accepted: December 07, 2017 95 The first attempts1 to document Greek folk songs in texts by both Greeks and foreigners included references to, or descriptions of, lament practices. -
Download Bibliography As .Pdf
BIBLIOGRAPHY BY SITE A Aetos http://www.yppo.gr/0/anaskafes/pdfs/LB_EPKA.pdf Agia Kyriaki Dakaris, S. (1972), Θεσπρωτία (Athens: Athens Centre of Ekistics). Agioi Apostoloi http://www.yppo.gr/0/anaskafes/pdfs/IB_EPKA.pdf Agios Donatos Forsén, B. (2011), 'Catalogue of Sites in the Central Kokytos Valley', in B. Forsén and E. Tikkala (eds.), Thesprotia expedition II, Environment and settlement patterns (Helsinki), 73-122. http://www.finninstitute.gr/en/thesprotia# 'Thesprotia Expedition 2004-5, Reports' Agios Georgios Dakaris, S. (1971), Cassopaia and the Elean colonies (Athens: Athens Center of Ekistics). Agios Minas Dausse, M.P. (2007), 'Les villes molosses: bilan et hypothèses sur les quatre centres mentionnés par Tite-Live', in D. Berranger-Auserve (ed.), Épire, Illyrie, Macédoine: Mélanges offerts au Professeur Pierre Cabanes (Clermont-Ferrand), 197-233. http://listedmonuments.culture.gr/fek.php?ID_FEKYA=12769 Agora (fortification and graves) Dakaris, S. (1972), Θεσπρωτία (Athens: Athens Centre of Ekistics). Agora PS29, PS30 and PS49 Forsén, B. (2011), 'Catalogue of Sites in the Central Kokytos Valley', in B. Forsén and E. Tikkala (eds.), Thesprotia expedition II, Environment and settlement patterns (Helsinki), 73-122. Almoutses Youni, P., Katsadima, I., and Faklari, I. (2001-4), 'Θέση Αλμούτσες, Κοινότητα Σελλάδων', Archaiologikon Deltion, 56-59 (B), 131-33. Alpochori Dakaris, S. (1971), Cassopaia and the Elean colonies (Athens: Athens Center of Ekistics). Amantia Anamali, S. (1972), 'Amantia', Iliria, II, 67-148. Cabanes, Pierre, et al. (2008), Carte archéologique de l'Albanie (Tirana: Klosi & Benzenberg). Ceka, N. (1990), 'Städtebau in der vorrömischen Periode in Südillyrien', Akten des XIII. Internationalen Kongresses für klassische Archäologie, Berlin, 1988 International Congress of Classical Archaeology (Mainz: Philipp von Zabern), 215-29. -
Hydroxyapatite and Fluorapatite in Conservative Dentistry and Oral Implantology—A Review
materials Review Hydroxyapatite and Fluorapatite in Conservative Dentistry and Oral Implantology—A Review Kamil Pajor, Lukasz Pajchel and Joanna Kolmas * Analytical Group, Department of Analytical Chemistry and Biomaterials, Faculty of Pharmacy with Laboratory Medicine Division, Medical University of Warsaw, 02-097 Warsaw, Poland * Correspondence: [email protected] Received: 29 July 2019; Accepted: 20 August 2019; Published: 22 August 2019 Abstract: Calcium phosphate, due to its similarity to the inorganic fraction of mineralized tissues, has played a key role in many areas of medicine, in particular, regenerative medicine and orthopedics. It has also found application in conservative dentistry and dental surgery, in particular, as components of toothpaste and mouth rinse, coatings of dental implants, cements, and bone substitute materials for the restoration of cavities in maxillofacial surgery. In dental applications, the most important role is played by hydroxyapatite and fluorapatite, i.e., calcium phosphates characterized by the highest chemical stability and very low solubility. This paper presents the role of both apatites in dentistry and a review of recent achievements in the field of the application of these materials. Keywords: hydroxyapatite; fluorapatite; dentistry; calcium phosphates 1. Introduction In recent decades, one has been able to observe huge progress in the field of dentistry. This results not only from the development of dental techniques and methods of therapy but also from significant developments in biomaterial engineering. The science of biomaterials is constantly increasing due to innovative modifications of already known materials or completely new biomaterials for applications in dentistry. Biodegradable polymers, bioactive ceramics, bioglass or metals covered with a layer of material facilitating osseointegration and, above all, composite materials are the main directions in the development of dental biomaterials [1–4]. -
Evaluation of a Fluorapatite-Spinel Ceramic As a Bone Implant Denginur Aksaci Iowa State University
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1981 Evaluation of a fluorapatite-spinel ceramic as a bone implant Denginur Aksaci Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Materials Science and Engineering Commons Recommended Citation Aksaci, Denginur, "Evaluation of a fluorapatite-spinel ceramic as a bone implant " (1981). Retrospective Theses and Dissertations. 6961. https://lib.dr.iastate.edu/rtd/6961 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This was produced from a copy of a document sent to us for microfilming. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the material submitted. The following explanation of techniques is provided to help you understand markings or notations which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to ubtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting through an image and duplicating adjacent pages to assure you of complete continuity. 2. When an image on the film is obliterated with a round black mark it is an indication that the film inspector noticed either blurred copy because of movement during exposure, or duplicate copy. -
Phosphorus-From Discovery to Commodity
Indian Journal of Chemical Technology Vol. 12, January 2005, pp. 108-122 Phosphorus-From discovery to commodity Jaime Wisniak* Department of Chemical Engineering, Ben-Gurion University of the Negev, Beer-Sheva, Israel 84105 Phosphorus is nearly the most widely and evenly distributed element on the surface of the earth, and probably the most subdivided. From a laboratory curiosity in the seventeeth century, it became recognized as a fundamental element of life and a large chemical commodity, improving agriculture and industry like very few other discoveries by men have done. Discovery of phosphorus nor the phenomenon was really new. Organic Mankind has been aware of luminiscent phosphorescent materials were known to Aristotle, phenomena for thousands of years; they are and a lithophosphorus was the subject of a book mentioned in different mythology and in the Bible. published in 1640, based on a discovery made by a Glowworms and fireflies, and the luminescent shoemaker, Vicenzo Casciarol, on Mons Padernus, organisms in sea water or on decaying fish and wood near Bologna in 16303. Casciarol claimed that the were long familiar sights and attracted the curiosity of stone was so heavy that he thought it contained a men. The Greeks called the planet Venus by the name heavy metal and that after it had been calcined in Phosphorus (morning star, from the Greek φϖζ = charcoal fire and cooled, it glowed in the darkness light + φερω = to bear), because it was visible before with a reddish light. The stone was called sunrise and after sundown. Venus took the name litheosphorus and also Bologna stone or lapis phosphorus in the morning and Hesperus in the bononiensis. -
Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective
The Principal Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective Gd Pr Ce Sm La Nd Scientific Investigations Report 2010–5220 U.S. Department of the Interior U.S. Geological Survey Cover photo: Powders of six rare earth elements oxides. Photograph by Peggy Greb, Agricultural Research Center of United States Department of Agriculture. The Principal Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective By Keith R. Long, Bradley S. Van Gosen, Nora K. Foley, and Daniel Cordier Scientific Investigations Report 2010–5220 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. Geological Survey, Reston, Virginia: 2010 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This report has not been reviewed for stratigraphic nomenclature. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Long, K.R., Van Gosen, B.S., Foley, N.K., and Cordier, Daniel, 2010, The principal rare earth elements deposits of the United States—A summary of domestic deposits and a global perspective: U.S. -
A Journey of the Vocal Iso(N)
A Journey of the Vocal Iso(n) A Journey of the Vocal Iso(n) By Eno Koço A Journey of the Vocal Iso(n) By Eno Koço This book first published 2015 Cambridge Scholars Publishing Lady Stephenson Library, Newcastle upon Tyne, NE6 2PA, UK British Library Cataloguing in Publication Data A catalogue record for this book is available from the British Library Copyright © 2015 by Eno Koço All rights for this book reserved. No part of this book may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior permission of the copyright owner. ISBN (10): 1-4438-7067-6 ISBN (13): 978-1-4438-7067-2 This book is dedicated to the memory of my mother, Albanian soprano Tefta Tashko Koço (1910–1947), who has been a mentor, an inspiration, and a guardian angel throughout my whole life and to whom I shall be eternally grateful TABLE OF CONTENTS List of Music Examples: Notation and Audio ........................................... ix List of Illustrations .................................................................................... xi Preface ..................................................................................................... xiii Acknowledgements ................................................................................ xvii Introduction ............................................................................................. xix Part I: Synthesis Chapter One ................................................................................................ -
The Turquoise-Chalcosiderite-Planerite
СПИСАНИЕ НА БЪЛГАРСКОТО ГЕОЛОГИЧЕСКО ДРУЖЕСТВО, год. 80, кн. 3, 2019, с. 48–50 REVIEW OF THE BULGARIAN GEOLOGICAL SOCIETY, vol. 80, part 3, 2019, p. 48–50 Национална конференция с международно участие „ГЕОНАУКИ 2019“ National Conference with international participation “GEOSCIENCES 2019” The turquoise-chalcosiderite-planerite solid-solution series in samples from Chala deposit, Eastern Rhodopes Тюркоаз-халкосидерит-планеритова серия от твърди разтвори в образци от находище Чала, Източни Родопи Yana Tzvetanova1, Louiza Dimowa1, Elena Tacheva1, Iskra Piroeva2, Ognyan Petrov1, Aleksandar Nikolov1 Яна Цветанова1, Луиза Димова1, Елена Тачева1, Искра Пироева2, Огнян Петров1, Александър Николов1 1 Institute of Mineralogy and Crystallography, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., bl. 107, 1113 Sofia, Bulgaria; E-mail: [email protected] 2 Institute of Physical Chemistry, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., bl. 11, 1113 Sofia, Bulgaria Keywords: turquoise, chalcosiderite, planerite, crystal chemistry, phosphates. Introduction quoise was also reported from the Obichnik depos- it, Zvezdel-Pcheloyad ore field, Eastern Rhodopes The turquoise group, as redefined by Foord and (Kunov, Mandova, 1997). Taggart (1998), consists of 6 members: planerite, The present study aims to show the crystal chem- turquoise, faustite, aheylite, chalcosiderite and an istry of green mineral from the turquoise group from 2+ 3+ unnamed Fe –Fe analogue with the general for- Chala deposit (Spahievo ore field) with particular at- mula A0–1B6(PO4)4–x(PO3OH)x(OH)8 4H2O, where tention to planerite end-member that was approved 2+ x = 0–2. Blue turquoise has Cu at the A position and by the IMA CNMMN as a revalidated mineral in 3+ Al at the B position, whereas green⋅ chalcosiderite 1984.