Mineral Resource Assessment of Heavy Mineral, Beach-Placer Sandstone
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Applicability of Siberian Placer Mining Technology to Alaska
MIRL Report No. 89 Applicability- - of Siberian Placer Mining Technology to Alaska Dr. Frank J. Skudrzyk, Project Manager E++W Engineering Consultants 461 1 Dartmouth Fairbanks, Alaska James C,Barker U.S. Bureau of Mines Alaska Field Operations Cenkr Fairbanks. Alaska Daniel E. Walsh School of Mineral Engineering University of Alaska Fairbanks Fairbanks, Alaska Rocky MacDonald American Arctic Company Fairbanks, Alaska Library of Congress Cataloging in Publication Data Library of Congress Catalog Card Number: 9 1-6 1923 ISBN 0-911043-12-8 May, 1991 Published bv Mined Industry Research Laboratory 212 ONeill Building University of Alaska Fairbanks Fairbanks, Alaska 99775-1 180 Alaska Science and Technology Foundation 550 West 7th Avenue Suite 360 Anchorage, Alaska 99501 ABSTRACT The result of Perestroyka and Glasnost has been an awakening of potential for cooperation between East and West. Nowhere has that been better demonstrated than between Alaska and Magadan Province, USSR. This report summarizes a one year effort financed by ASTF, with participation from several technical organizations, to establish contacts with the Siberian placer mining industry. The purpose of the project was to provide initial assessment of the Soviet technology for placer mining in permafrost. A ten day trip to Magadan province by an ASTF team and a similar length visit to Alaska by the Soviet mining group representing the All Union Scientific and Research Institute of Gold and Rare Metals, (VNII-I), Magadan are described. The report also reviews translated data on mining in permafrost and describes surface and underground placer mining technology developed by the Soviets. The report also lists relevant publications on Soviet mining research and state of the art Soviet mining technology and expertise. -
Hawaiian Volcanoes US$1225
The Geological Society of America’s Explore Hawaiian Volcanoes FIELD EXPERIENCE 27 July - 4 August 2014 Experience the wonders of active volcanism on the Earth’s most accessable and active volcano - Kilauea on the Big Island of Hawaii! This eight-day field trip on the Big Island of Hawaii will expand your knowl- edge in the field of plate tectonics, hot spot volcanism and the geologic features and hazards associated with living on an active volcano. We will discuss volcanic edifices, eruption styles, magma evolution and see various types of lava flows, lava lakes, tree molds and lava trees, fault scarps, rifts, craters and calderas. We will use our observations and new- found knowledge to discuss methods on how to effectively communicate geologic concepts. We will model inquiry in the field. US Prince does not include$1225 airfares to/from Hilo, HI. Trip ITINERARY* Sunday, July 27 - Participants arrive in Hilo, Hawaii for transfer via van to Kilauea Military Camp. No meals pro- vided. We will go to dinner as a group at Ken’s House of Pancakes (at your own expense) Monday, July 28 - Overview/logistics, Kilauea Visitor Center, Steaming Bluffs, Sulphur Banks, Kilauea Overlook, HVO, Jaggar Museum, SW Rift, Halema’uma’u Overlook (if open), Keanakako’I overlook, Devastation Trail, Pu’u Pua’i Overlook. ~ 4 miles of hiking on easy trails. BLD. Tuesday, July 29 - Chain of Craters Road including stops at Lua Manu Crater, Pauahi Crater and others, Mauna Ulu trail to Pu’u Huluhulu, Kealakomo Overlook, Alanui Kahiko, P’u Loa Petroglyphs, Holei Sea Arch, end of Chain of Craters Road. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Exploration of Placer Gold Deposits by Geomagnetic Surveys
MTR-2 EXPLORATION OF PLACER GOLD DEPOSITS BY GEOMAGNETIC SURVEYS by Eric Anderson V. P. Exploration Placer Management Group, Ltd. EXPLORATION OF PLACER GOLD DEPOSITS BY GEOMAGNETIC SURVEYS by Eric Anderson V. P. Exploration Placer Management Group, Ltd. Exploration of Placer Gold Deposits by Geomagnetic Surveys Eric Anderson, V.P. Exploration Placer Management Group, Ltd. ABSTRACT Past attempts to explore for placer gold deposits by measuring the anomalous magnetic intensities of the magnetite normally found in the ”black sands” fraction of placer gravels were for the most part unsuccessful. Recent improvements in the sensitivity, reliability and portability of magnetometers have made it possible to cheaply and accurately delineate some types of placer gravels if they occur in a geological environment that is ”magnetically hospitable” and does not mask the signal of the overlaying gravels. The main benefit of this technique is that it can accurately delineate targets and thus dramatically reduce the overall cost of an exploration program in a given area. INTRODUCTION Whether or not this technique will work in a given area depends on three factors: 1. The amount of magnetite associated with the pay gravels. 2. The depth of the gravel deposit. 3. The nature of the underlying bedrock. In our work to date in Western Canada and United States, we have not encountered any pay gravels that did not have measurable concentrations of magnetite in the black sands. It is common to find gravel deposits with high concentrations of magnetite and no gold values whatsoever, but our experience and history have shown that gold values rarely occur without associated magnetic black sands; although the concentrates of magnetite do vary tremendously, In this regard it is important to keep two things in mind: 1. -
COMPARATIVE STUDIES on the BLACK SAND CONCENTRATES of SOUTH INDIA by Dr
COMPARATIVE STUDIES ON THE BLACK SAND CONCENTRATES OF SOUTH INDIA BY Dr. E. A. V. PRASAD [Department oJ Geology, Sri Venkateswara University, Tirupati (A.P.), Indic] Received June 24, 1971 (Communicated by Dr. K. Neelakantam, F.A.SC.) ABSTRACT Samples of the littoral and alluvial placer deposits of the black sand concentrates which contain radioactive resistate minerals were collected from various parts of South India and their characters with respect to colour, density and radioactivity were presented. With the aid of a hand magnet and a sensitive Frantz Isodynamic laboratory model Lj magnetic separator, each sample was subdivided into magnetic, paramagnetic and nonmagnetic components. The paramagnetic mineral assemblage was further subdivided into fractions of varying mass magnetic susceptibility. The amounts of these fractions constitute the frequency distribution of mass magnetic susceptibility, expressed in terms of current strength, of the sample whose character is ttien evaluated by means of certain standard statistical parameters. Variation in the characters with respect to grain size was also studied. Fm'ther, it is suggested that the amount of magnetite is an "Index of Maturity" for these residual deposits. THE voluminous black sand concentrates occurring along the East and West coasts of India, in a series of local concentrations, at favourable localities, constitute a thorium asset of world importance. These placer deposits contain the radioactive mineral, monazite, together with the other industrial minerals ilmenite, garnet, rutile, zircon, magnetite and leucoxene in varying proportions. Such placer deposits of radioactive resistate minerals have been reported from many parts of the world (Nininger,1954; United Nations, 1956; Heinrich, 1958). -
ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006
ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006 Massachusetts Institute of Technology/ Woods Hole Oceanographic Institution Joint Program in Oceanography This field trip guide was compiled by Karen L. Bice using information from Bryndís Brandsdóttir, Richard S. Williams, Helgi Torfason, Helgi Bjornsson, Oddur Sigurðsson, the Iceland Tourist Board and World W. Web Maps from Thordarson and Hoskuldsson, 2002, Iceland (Classic Geology in Europe 3), Terra Publishing, UK. Logistical genius: Andrew T. Daly Field trip participants: Mark Behn, Karen Bice, Roger Buck, Andrew Daly, Henry Dick, Hans Schouten, Martha Buckley, James Elsenbeck, Pilar Estrada, Fern Gibbons, Trish Gregg, Sharon Hoffmann, Matt Jackson, Michael Krawczynski, Christopher Linder, Johan Lissenberg, Andrea Llenos, Rowena Lohman, Luc Mehl, Christian Miller, Ran Qin, Emily Roland, Casey Saenger, Rachel Stanley, Peter Sugimura, and Christopher Waters The Geodynamics Program is co-sponsored by Woods Hole Oceanographic Institution’s Academic Programs Office and Deep Ocean Exploration Institute. TUESDAY May 30 Estimated driving (km) Meet at Logan Airport, Icelandair ticket counter @ 7:00 PM (80 km ≈ 50 mi) Depart BOS 9:30 PM Icelandair flight Day 1 - WEDNESDAY May 31 Arrive Keflavík International Airport 6:30 AM (flight duration 5 hours) Pick up 2 vans, 2 trailers (Budget) Free day in Reykjavík Night @ Laugardalur campground, Reykjavík Dinner: on own in town Day 2 - THURSDAY June 1 270 Late start due to trailer problems (2 hrs @ AVIS) To Þingvellir N.P., then north to Hvalfjörður fjord, stop at Skorradalsvatn Night @ Sæberg Hostel (1 km. off Rte 1 in Hrútafjörður, west side of road) Tel. 354-4510015 Fax. 354-4510034 [email protected] Dinner: mexican-style chicken (Rachel, Trish, Chris) Day 3 - FRIDAY June 2 320 To Lake Myvatn Lunch stop in Akureyri, stop at Godafoss, stop at Skutustadir pseudocraters Night @ Ferdathjonustan Bjarg campsite, Reykjahlid, on shore of Lake Myvatn Tel. -
Gold, Platinum and Diamond Placer Deposits in Alluvial Gravels, Whitecourt, Alberta Special Report 89
Special Report 89 Gold, Platinum and Diamond Placer Deposits in Alluvial Gravels, Whitecourt, Alberta Special Report 89 Gold, Platinum and Diamond Placer Deposits in Alluvial Gravels, Whitecourt, Alberta G.G. Mudaliar1, J.P. Richards1 and D.R Eccles2 1 Department of Earth & Atmospheric Sciences, University of Alberta 2 Alberta Geological Survey May 2007 ©Her Majesty the Queen in Right of Alberta, 2007 ISBN 0-7785-3851-6 The Alberta Geological Survey and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness, or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions (specified in 'Licence Agreement for Digital Products'"). The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release does not constitute endorsement by the Alberta Geological Survey of any manufacturer's product. This product is an EUB/AGS Special Report; the information is provided as received from the author and has had minimal editing for conformity to EUB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the Alberta Geological Survey/Alberta Energy and Utilities Board. The following reference format is recommended: Mudaliar, G.G., Richards, J.P. and Eccles, D.R. (2007): Gold, platinum and diamond placer deposits in alluvial gravels, Whitecourt, Alberta; Alberta Energy and Utilities Board, EUB/AGS, SPE 089, 24 p. -
Colloform High-Purity Platinum from the Placer Deposit
Colloform high-purity platinum from the placer deposit of Koura River (Gornaya Shoriya, Russia) Nesterenko G.V.1, Zhmodik S.M.1,2, Airiyants E.V.1, Belyanin D.K.1,2, Kolpakov V.V.1, Bogush A.A.1,3,* 1V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Novosibirsk 630090, Russia 2Novosibirsk State University, Novosibirsk 630090, Russia 3Department of Civil, Environmental & Geomatic Engineering, University College London, London WC1E 6BT, UK *Corresponding author: A.A. Bogush, E-mail: [email protected] Abstract A microinclusion of colloform high-purity platinum in a grain of platinum-group minerals (PGM) from the alluvial gold-bearing placer deposit in the south of Western Siberia (Russia) was detected and characterized for the first time. It is different in composition, texture, and conditions of formation from high-purity platinum of other regions described in the literature. The main characteristics of investigated high-purity platinum are colloform-layered texture, admixture of Fe (0.37-0.78 wt.%), and paragenesis of Cu-rich isoferroplatinum, hongshiite, and rhodarsenide. The PGM grain with high-purity platinum is multiphase and heterogeneous in texture. It is a product of intensive metasomatic transformation of Cu-rich isoferroplatinum (Pt3(Fe0.6Cu0.4)). The transformation was carried out in two stages: 1 - copper stage including three substages (Cu-rich isoferroplatinum, copper platinum and hongshiite); and 2 - arsenic (rhodarsenide). The formation of high-purity platinum was separated in time from the formation of isoferroplatinum and was carried out by precipitation from postmagmatic solutions. Keywords: platinum-group elements (PGE), platinum-group minerals (PGM), high-purity platinum, Cu-rich isoferroplatinum, hongshiite, alluvial placer, Gornaya Shoriya Introduction High-purity platinum was discovered in the gold-bearing placer deposit of Koura River situated in Gornaya Shoriya (south-western Siberia, Russia, Fig. -
Mineralogy of Platinum-Group Elements and Gold in the Ophiolite-Related Placer of the River Bolshoy Khailyk, Western Sayans, Russia
minerals Article Mineralogy of Platinum-Group Elements and Gold in the Ophiolite-Related Placer of the River Bolshoy Khailyk, Western Sayans, Russia Andrei Y. Barkov 1,*, Gennadiy I. Shvedov 2, Sergey A. Silyanov 2 and Robert F. Martin 3 1 Research Laboratory of Industrial and Ore Mineralogy, Cherepovets State University, 5 Lunacharsky Avenue, 162600 Cherepovets, Russia 2 Institute of Mining, Geology and Geotechnology, Siberian Federal University, 95 Avenue Prospekt im. gazety “Krasnoyarskiy Rabochiy”, 660025 Krasnoyarsk, Russia; [email protected] (G.I.S.); [email protected] (S.A.S.) 3 Department of Earth and Planetary Sciences, McGill University, 3450 University Street, Montreal, QC H3A 0E8, Canada; [email protected] * Correspondence: [email protected]; Tel.: +7-8202-51-78-27 Received: 21 May 2018; Accepted: 5 June 2018; Published: 12 June 2018 Abstract: We describe assemblages of platinum-group minerals (PGM) and associated PGE–Au phases found in alluvium along the River Bolshoy Khailyk, in the western Sayans, Russia. The river drains the Aktovrakskiy ophiolitic complex, part of the Kurtushibinskiy belt, as does the Zolotaya River ~15 km away, the site of other placer deposits. Three groups of alloy minerals are described: (1) Os–Ir–Ru compositions, which predominate, (2) Pt–Fe compositions of a Pt3Fe stoichiometry, and (3) Pt–Au–Cu alloys, which likely crystallized in the sequence from Au–(Cu)-bearing platinum, Pt(Au,Cu), Pt(Cu,Au), and PtAuCu2, to PtAu4Cu5. The general trends of crystallization of PGM appear to be: [Os–Ir–Ru alloys] ! Pt3Fe-type alloy (with inclusions of Ru-dominant alloy formed by exsolution or via replacement of the host Pt–Fe phase) ! Pt–Au–Cu alloys. -
The Placer Gold Mining Game
The Placer Gold Mining Game Game designed by Rob Chapman, School of Earth and Environment, University of Leeds. Software designed by Matt Bindoff, Bindoff Media Top: Preparing to mine gold-bearing gravel in Sulphur Creek, Klondike District Yukon Canada. Below: a portable sluice retains the gold in the riffles Overview Welcome to this interactive computer game in which you get to make the decisions made by real placer miners. When you play the game there are instructions which provide you with various options and tell you what you can and cannot do. To give yourself the best chance at the game you have to understand something about placer gold: how it occurs, how you find out if there is any there at all and how you can recover it. The object of the game, (of course) is to make as much profit as you can. You gain cash by selling the gold that you recover, but everything that you do to find, mine and separate the gold from the gravel cost you either time, money, or both. As far as possible we have made the game faithful to the real activity, so that you can make the same decisions and be faced with the same challenges that real placer miners encounter. However any real placer miners who have a go will quickly realize that we have had to make some simplifications to make the game workable in an educational context, (such as large claim sizes and a very understanding bank manager!) The key elements of the game can be summarized as follows: 1. -
Significant Metalliferous Lode Deposits and Placer Districts of Alaska
Significant Metalliferous Lode Deposits and Placer Districts of Alaska By WARREN J. NOKLEBERG, THOMAS K. BUNDTZEN, HENRY C. BERG, DAVID A. BREW, DONALD GRYBECK, MARK S. ROBINSON, THOMAS E. SMITH, and WARREN YEEND U.S. GEOLOGICAL SURVEY BULLETIN 1786 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1987 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-PublicationData Significant metalliferous lode deposits and placer districts of Alaska. U.S. Geological Survey Bulletin 1786 Bibliography Supt. of Docs. No.: 1 19.3:1786 1. Placer deposits-Alaska. 2. Ore deposits-Alaska. I. Nokleberg, Warren J. II. Series. QE75.B9 No. 1786 557.3 s 87-600165 [TN24.A4] [553'.13'09798] COVER Mill buildings at Kennecott, Alaska. The Kennecott district Cu-Ag mines in the Wrangell Mountains were some of the principal sources of copper in North America from 1913 to 1938. See deposit description for Kennecott district (number 30 for southern Alaska). Copyrighted drawing used by permission of Gail Niebrugge, artist, Glennallen, Alaska. PREFACE This report is a compilation of the signifi- geology. The unpublished data were contributed cant metalliferous lode deposits and placer by mineral deposit and regional geologists in districts of Alaska, and is a comprehensive data private industry, universities, the U.S. Geo- base for a companion article on the metallogene- logical Survey, the Alaska Division of Geologi- sis and major mineral deposits of Alaska that cal and Geophysical Surveys, the U.S. -
Study of Black Sand Particles from Sand Dunes in Badr, Saudi Arabia Using Electron Microscopy
Atmosphere 2015, 6, 1175-1194; doi:10.3390/atmos6081175 OPEN ACCESS atmosphere ISSN 2073-4433 www.mdpi.com/journal/atmosphere Article Study of Black Sand Particles from Sand Dunes in Badr, Saudi Arabia Using Electron Microscopy Haider Abbas Khwaja 1,2,*, Omar Siraj Aburizaiza 3,*, Daniel L. Hershey 4, Azhar Siddique 3,5, David A. Guerrieri P. E. 4, Jahan Zeb 3, Mohammad Abbass 6, Donald R. Blake 7, Mirza Mozammel Hussain 1,2, Abdullah Jameel Aburiziza 8, Malissa A. Kramer 4 and Isobel J. Simpson 7 1 Wadsworth Center, New York State Department of Health, Albany, New York, NY 12201, USA; E-Mail: [email protected] 2 Department of Environmental Health Sciences, School of Public Health, University at Albany, Albany, New York, NY 12201, USA 3 Unit for AinZubaida and Groundwater Research, King Abdulaziz University, Jeddah 21589, Saudi Arabia; E-Mails: [email protected] (A.S.); [email protected] (J.Z.) 4 New York State Department of Environmental Conservation, 625 Broadway, Albany, New York, NY 12233, USA; E-Mails: [email protected] (D.L.H.); [email protected] (D.A.G.P.E.); [email protected] (M.A.K.) 5 Chemistry Department, University of Karachi, Karachi 75270, Pakistan 6 Civil Engineering Department, King Abdulaziz University, Jeddah 21589, Saudi Arabia; E-Mail: [email protected] 7 Department of Chemistry, University of California-Irvine, Irvine, CA 92697, USA; E-Mails: [email protected] (D.R.B.); [email protected] (I.J.S.) 8 School of Medicine, Umm Ul Qura University, Mecca 21955, Saudi Arabia; E-Mail: [email protected] * Authors to whom correspondence should be addressed; E-Mails: [email protected] (H.A.K.); [email protected] (O.S.A.); Tel.: +1-518-474-0516 (H.A.K.); +966-12-695-2821 (O.S.A.); Fax: +1-518-473-2895 (H.A.K.); +966-12-695-2499 (O.S.A.).