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US Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR *"! ' 5, GEOLOGICAL SURVEI PEGMATITE GEOLOGY OF THE SHELBY DISTRICT NORTH CAROLINA by \ Wallace R. Griffitts > \ I ,' -* U. S. Geological Survey ' ' OPEN FILE REPORT 5 Ihis report is preliminary and has not been edited or reviewed for conformity with Geological Suj'V*-'/ standards or nomenclature. COHTEHTS _ _ - Page Abstract Introduction. ........................... 1 Location and physical features ................ 1 Field work and acknowledgments ................ 2 Geology .............................. k Metamorphic rocks....................... h- Carolina gneiss ..................... Ij- General features .................. ^4- Lithology. ..................... k Biotite gneiss member. ............... 6 Battleground schist ................... 9 General features .................. 9 Lithology. ..................... 9 Hornblende schist and gneiss. .............. 11 General features .................. 11 Gabbroic rocks ................... 11 Hornblende schists ................. 13 Pyroxenite and associated rocks. .......... 13 Schist and granite complex. ................ 14- Igneous rocks. ........................ 15 Toluca quartz monzonite ................. 15 . : .r *- General features .................. 15 ^ c Lithology. ..................... 16 Yorkville granite .................... 19 General features .................. 19 Lithology. ..................... 20 Page CherryvlUe quartz monzonite. ............. 20 General features ................. 20 Relations to enclosing rocks ........... 23 Lithology. -
Pezzottaite from Ambatovita, Madagascar: a New Gem Mineral
PEZZOTTAITE FROM AMBATOVITA, MADAGASCAR: A NEW GEM MINERAL Brendan M. Laurs, William B. (Skip) Simmons, George R. Rossman, Elizabeth P. Quinn, Shane F. McClure, Adi Peretti, Thomas Armbruster, Frank C. Hawthorne, Alexander U. Falster, Detlef Günther, Mark A. Cooper, and Bernard Grobéty Pezzottaite, ideally Cs(Be2Li)Al2Si6O18, is a new gem mineral that is the Cs,Li–rich member of the beryl group. It was discovered in November 2002 in a granitic pegmatite near Ambatovita in cen- tral Madagascar. Only a few dozen kilograms of gem rough were mined, and the deposit appears nearly exhausted. The limited number of transparent faceted stones and cat’s-eye cabochons that have been cut usually show a deep purplish pink color. Pezzottaite is distinguished from beryl by its higher refractive indices (typically no=1.615–1.619 and ne=1.607–1.610) and specific gravity values (typically 3.09–3.11). In addition, the new mineral’s infrared and Raman spectra, as well as its X-ray diffraction pattern, are distinctive, while the visible spectrum recorded with the spec- trophotometer is similar to that of morganite. The color is probably caused by radiation-induced color centers involving Mn3+. eginning with the 2003 Tucson gem shows, (Be3Sc2Si6O18; Armbruster et al., 1995), and stoppaniite cesium-rich “beryl” from Ambatovita, (Be3Fe2Si6O18; Ferraris et al., 1998; Della Ventura et Madagascar, created excitement among gem al., 2000). Pezzottaite, which is rhombohedral, is Bcollectors and connoisseurs due to its deep purplish not a Cs-rich beryl but rather a new mineral species pink color (figure 1) and the attractive chatoyancy that is closely related to beryl. -
Redalyc.Mineralogical Study of the La Hueca Cretaceous Iron-Manganese
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Corona Esquivel, Rodolfo; Ortega Gutiérrez, Fernando; Reyes Salas, Margarita; Lozano Santacruz, Rufino; Miranda Gasca, Miguel Angel Mineralogical study of the La Hueca Cretaceous Iron-Manganese deposit, Michoacán, south-western Mexico Revista Mexicana de Ciencias Geológicas, vol. 17, núm. 2, 2000, pp. 142-151 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57217206 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas, volumen 17, número 2, 143 2000, p. 143- 153 Universidad Nacional Autónoma de México, Instituto de Geología, México, D.F MINERALOGICAL STUDY OF THE LA HUECA CRETACEOUS IRON- MANGANESE DEPOSIT, MICHOACÁN, SOUTHWESTERN MEXICO Rodolfo Corona-Esquivel1, Fernando Ortega-Gutiérrez1, Margarita Reyes-Salas1, Rufino Lozano-Santacruz1, and Miguel Angel Miranda-Gasca2 ABSTRACT In this work we describe for the first time the mineralogy and very briefly the possible origin of a banded Fe-Mn deposit associated with a Cretaceous volcanosedimentary sequence of the southern Guerrero terrane, near the sulfide massive volcanogenic deposit of La Minita. The deposit is confined within a felsic tuff unit; about 10 meters thick where sampled for chemical analysis. Using XRF, EDS and XRD techniques, we found besides todorokite, cryptomelane, quartz, romanechite (psilomelane), birnessite, illite-muscovite, cristobalite, chlorite, barite, halloysite, woodruffite, nacrite or kaolinite, and possibly hollandite-ferrian, as well as an amorphous material and two unknown manganese phases. -
Mineral Industries and Geology of Certain Areas
REPORT -->/ OF TFIE STATE GEOLOGIST ON THE S 7 (9 Mineral Industries and Geology 12 of Certain Areas OF -o VERMONT. 'I 6 '4 4 7 THIRD OF THIS SERIES, 1901-1902. 4 0 4 S GEORGE H. PERKINS, Ph. D., 2 5 State Geologist and Professor of Geology, University of Vermont 7 8 9 0 2 4 9 1 T. B. LYON C0MI'ANV, I'RINTERS, ALILiNY, New VORK. 1902. CONTENTS. PG K 1NTRODFCTION 5 SKETCH OF THE LIFE OF ZADOCK THOMPSON, G. H. Perkins ----------------- 7 LIST OF OFFICIAL REPORTS ON VERMONT GEOLOGY ----------------- -- -- ----- 14 LIST OF OTHER PUBLICATIONS ON VERMONT GEOLOGY ------- - ---------- ----- 19 SKETCH OF THE LIFE OF AUGUSTUS WING, H. M. Seely -------------------- -- 22 REPORT ON MINERAL INDUSTRIES, G. H. Perkins ............................ 35 Metallic Products ------------------------------------------------------ 32 U seful Minerals ------------------------------------------------------- 35 Building and Ornamental Stone ----------------------------------------- 40 THE GRANITE AREA OF BAItRE, G. I. Finlay------------------------------ --- 46 Topography and Surface Geology ------------------------------------ - -- 46 General Geology, Petrography of the Schists -------------------------- - -- 48 Description and Petrography of Granite Areas ----------------------------51 THE TERRANES OF ORANGE COUNTY, VERMONT, C. H. Richardson ------------ 6i Topography---------------------------- -............................. 6z Chemistry ------------------------------------------------------------66 Geology -------------------------------------------------------------- -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
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. -
Structural Analysis of Precambrian Metasedimentary Rocks of the Swede Gulch Formation, Nahant, South Dakota
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1981 Structural Analysis of Precambrian Metasedimentary Rocks of the Swede Gulch Formation, Nahant, South Dakota Richard G. Cookman Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Cookman, Richard G., "Structural Analysis of Precambrian Metasedimentary Rocks of the Swede Gulch Formation, Nahant, South Dakota" (1981). Master's Theses. 1837. https://scholarworks.wmich.edu/masters_theses/1837 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. STRUCTURAL ANALYSIS OF PRECAMBRIAN METASEDIMENTARY ROCKS OF THE SWEDE GULCH FORMATION, NAHANT, SOUTH DAKOTA by Richard G. Coohman A Thesis Submitted to the Faculty of the Graduate College in partial fulfillment of the requirenents for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan December 1981 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. STRUCTURAL ANALYSIS OF PRECAMBRIAN METASEDIMENTARY ROCKS OF THE SWEDE GULCH FORMATION, NAHANT, SOUTH DAKOTA Richard G. Cookman, M.S. Western Michigan University, 1981 Precambrian X tectonites deformed between thermal domes in the northern Black Hills 1.7 B.Y.B.P. display variably trending isoclinal folds cross-cut by southeast trending slip-folds developed in discrete shear zones. Eugeosynclinal sedimentary rocks consisting of shale, quartzarenite , sublitharenite, and graywacke were meta morphosed to phyllite, quartzite, and metagraywacke during two syntectonic phases and one post-tectonic phase. -
MINERALOGY for PETROLOGISTS Comprising a Guidebook and a Full Color CD-ROM, This Reference Set Offers Illustrated Essentials to Study Mineralogy, Applied to Petrology
MINERALOGY for PETROLOGISTS for MINERALOGY Comprising a guidebook and a full color CD-ROM, this reference set offers illustrated essentials to study mineralogy, applied to petrology. While there are some excellent reference works available on this subject, this work is unique for its data richness and its visual character. MINERALOGY for PETROLOGISTS With a collection of images that excels both in detail and aesthetics, 151 minerals are presented in more than 400 plates. Different facies and paragenesis, both in natural polarized light, are shown for every mineral and optical data, sketches of the crystal habitus, chemical composition, occurrence and a brief description are Optics, Chemistry and Occurrences included. The accompanying user guide gives a general introduction to microscope mineral observation, systematic mineralogy, mineral chemistry, occurrence, of Rock-Forming Minerals stability, paragenesis, structural formula calculation and its use in petrology. This compact set will serve as a field manual to students, researchers and Michel Demange professionals in geology, geological, mining, and mineral resources engineering to observe and determine minerals in their studies or field work. Dr. Michel Demange has devoted his career to regional geology and tectonics of metamorphic and magmatic terranes and to ore deposits. Graduated from the École Nationale Supérieure des Mines de Paris and holding a Docteur-es-Sciences from the University Pierre et Marie Curie, Paris VI, he has been active in a rich variety of geological projects and investigations around the world. In combination with his teaching and research activities at the École des Mines in Paris, France, he headed various research studies. This book benefits from the great experience in field M. -
Summer 2007 Gems & Gemology Gem News
EDITOR Brendan M. Laurs ([email protected]) CONTRIBUTING EDITORS Emmanuel Fritsch, IMN, University of Nantes, France ([email protected]) Henry A. Hänni, SSEF, Basel, Switzerland ([email protected]) Franck Notari, GemTechLab, Geneva, Switzerland ([email protected]) Kenneth V. G. Scarratt, GIA Research, Bangkok, Thailand ([email protected]) DIAMONDS U.S. Patent and Trademark Office (USPTO) awards patents, and consequently it may affect the validity of a Bar code technology applied to diamonds. Inscribing dia- number of patents on diamond cut designs. monds using lasers and other technologies has become a A general review of U.S. patent law as it applies to routine method for identifying a stone and personalizing it diamond cuts can be found in the Winter 2002 G&G (T. for individual situations. At the same time, bar coding has W. Overton, “Legal protection for proprietary diamond evolved from the traditional one-dimensional array of lines cuts,” pp. 310–325). One of the factors that the USPTO to a two-dimensional matrix code that can hold far more considers in awarding a patent is whether the claimed information. invention is a development that would be “obvious” to Diamond laser inscription technology has now pro- a person having ordinary skill in the relevant field. An gressed to the point where a miniature matrix code can be obvious invention is not eligible for a patent. Until the inscribed on the girdle of a diamond (see, e.g., figure 1). KSR International case, the U.S. Court of Appeals for Instead of just a grading report number, the matrix code the Federal Circuit (which has jurisdiction over patent can store all of the information in the report itself, such as disputes) applied a fairly narrow definition of obvious- clarity, cut, and color grades, as well as country of origin (if ness: whether a specific motivation or suggestion to known), the name of the manufacturer, and other combine prior inventions or knowledge (referred to as specifics. -
Winter 2003 Gems & Gemology
Winter 2003 VOLUME 39, NO. 4 EDITORIAL _____________ 267 Tomorrow’s Challenge: CVD Synthetic Diamonds William E. Boyajian FEATURE ARTICLES _____________ 268 Gem-Quality Synthetic Diamonds Grown by a Chemical Vapor Deposition (CVD) Method Wuyi Wang, Thomas Moses, Robert C. Linares, James E. Shigley, Matthew Hall, and James E. Butler pg. 269 Description and identifying characteristics of Apollo Diamond Inc.’s facetable, single-crystal type IIa CVD-grown synthetic diamonds. 284 Pezzottaite from Ambatovita, Madagascar: A New Gem Mineral Brendan M. Laurs, William B. (Skip) Simmons, George R. Rossman, Elizabeth P. Quinn, Shane F. McClure, Adolf Peretti, Thomas Armbruster, Frank C. Hawthorne, Alexander U. Falster, Detlef Günther, Mark A. Cooper, and Bernard Grobéty A look at the history, geology, composition, and properties of this new cesium-rich member of the beryl group. 302 Red Beryl from Utah: A Review and Update James E. Shigley, Timothy J. Thompson, and Jeffrey D. Keith A report on the geology, history, and current status of the world’s only known occurrence of gem-quality red beryl. pg. 299 REGULAR FEATURES _____________________ 314 Lab Notes • Chrysocolla “owl” agate • Red coral • Coated diamonds • Natural emerald with nail-head spicules • Emerald with strong dichroism • High-R.I. glass imitation of tanzanite • Large clam “pearl” • Blue sapphires with unusual color zoning • Spinel with filled cavities 322 Gem News International • Comparison of three historic blue diamonds • Natural yellow diamond with nickel-related optical centers -
INTERNATIONAL GEMMOLOGICAL CONFERENCE Nantes - France INTERNATIONAL GEMMOLOGICAL August 2019 CONFERENCE Nantes - France August 2019
IGC 2019 - Nantes IGC 2019 INTERNATIONAL GEMMOLOGICAL CONFERENCE Nantes - France INTERNATIONAL GEMMOLOGICAL August 2019 CONFERENCE Nantes - France www.igc-gemmology.org August 2019 36th IGC 2019 – Nantes, France Introduction 36th International Gemmological Conference IGC August 2019 Nantes, France Dear colleagues of IGC, It is our great pleasure and pride to welcome you to the 36th International Gemmological Conference in Nantes, France. Nantes has progressively gained a reputation in the science of gemmology since Prof. Bernard Lasnier created the Diplôme d’Université de Gemmologie (DUG) in the early 1980s. Several DUGs or PhDs have since made a name for themselves in international gemmology. In addition, the town of Nantes has been on several occasions recognized as a very attractive, green town, with a high quality of life. This regional capital is also an important hub for the industry (e.g. agriculture, aeronautics), education and high-tech. It has only recently developed tourism even if has much to offer, with its historical downtown, the beginning of the Loire river estuary, and the ocean close by. The organizers of 36th International Gemmological Conference wish you a pleasant and rewarding conference Dr. Emmanuel Fritsch, Dr. Nathalie Barreau, Féodor Blumentritt MsC. The organizers of the 36th International Gemmological Conference in Nantes, France From left to right Dr. Emmanuel Fritsch, Dr. Nathalie Barreau, Féodor Blumentritt MsC. 3 36th IGC 2019 – Nantes, France Introduction Organization of the 36th International Gemmological Conference Organizing Committee Dr. Emmanuel Fritsch (University of Nantes) Dr. Nathalie Barreau (IMN-CNRS) Feodor Blumentritt Dr. Jayshree Panjikar (IGC Executive Secretary) IGC Executive Committee Excursions Sophie Joubert, Richou, Cholet Hervé Renoux, Richou, Cholet Guest Programme Sophie Joubert, Richou, Cholet Homepage Dr. -
General Index Vols. XLI-L, Third Series
GENERAL INDEX OF VOLUMES XLI-L OF THE THIRD SERIES. WInthe references to volumes xli to I, only the numerals i to ir we given. NOTE.-The names of mineral8 nre inaerted under the head ol' ~~IBERALB:all ohitllary notices are referred to under OBITUARY. Under the heads BO'PANY,CHK~I~TRY, OEOLO~Y, Roo~s,the refereuces to the topics in these department8 are grouped together; in many cases, the same references appear also elsewhere. Alabama, geological survey, see GEOL. REPORTSand SURVEYS. Abbe, C., atmospheric radiation of Industrial and Scientific Society, heat, iii, 364 ; RIechnnics of the i. 267. Earth's Atmosphere, v, 442. Alnska, expedition to, Russell, ii, 171. Aberration, Rayleigh, iii, 432. Albirnpean studies, Uhler, iv, 333. Absorption by alum, Hutchins, iii, Alps, section of, Rothpletz, vii, 482. 526--. Alternating currents. Bedell and Cre- Absorption fipectra, Julius, v, 254. hore, v, 435 ; reronance analysis, ilcadeiny of Sciences, French, ix, 328. Pupin, viii, 379, 473. academy, National, meeting at Al- Altitudes in the United States, dic- bany, vi, 483: Baltimore, iv, ,504 : tionary of, Gannett, iv. 262. New Haven, viii, 513 ; New York, Alum crystals, anomalies in the ii. 523: Washington, i, 521, iii, growth, JIiers, viii, 350. 441, v, 527, vii, 484, ix, 428. Aluminum, Tvave length of ultra-violet on electrical measurements, ix, lines of, Runge, 1, 71. 236, 316. American Association of Chemists, i, Texas, Transactions, v, 78. 927 . Acoustics, rrsearchesin, RIayer, vii, 1. Geological Society, see GEOL. Acton, E. H., Practical physiology of SOCIETYof AMERICA. plants, ix, 77. Nuseu~nof Sat. Hist., bulletin, Adams, F.