Source and Bedrock Distribution of Gold and Platinum-Group Metals in the Slate Creek Area, Northern.Chistochina Mining District, East-Central Alaska

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Geology of the Nimrod Area Granite County Montana

University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1958 Geology of the Nimrod area Granite County Montana Joel Kenneth Montgomery The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Montgomery, Joel Kenneth, "Geology of the Nimrod area Granite County Montana" (1958). Graduate Student Theses, Dissertations, & Professional Papers. 7095. https://scholarworks.umt.edu/etd/7095 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. aUv DATE DUE .**'“ '■’ K ^-r>o<> . t_A \J ^ D e c 0 1 ]ggg ^ A H 1 5 GEOLOGY OP THE NIMROD AREA GRANITE COUNTY, MONTANA by JOEL K. MONTGOMERY B. S. Brigham Young University, 1956 Presented in partial fulfillment of the requirements for the degree Master of Science MONTANA STATE UNIVERSITY 1958 Approved by: Chairman, Board of ^aminers Dean, Graduate School 2 0 1953 bate UMl Number: EP37896 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT OisMftartion Publishing UMl EP37896 Published by ProQuest LLC (2013).
Mineralogy and Geochemistry of Some Belt Rocks, Montana and Idaho

Mineralogy and Geochemistry of Some Belt Rocks, Montana and Idaho By J. E. HARRISON and D. J. GRIMES CONTRIBUTIONS TO ECONOMIC GEOLOGY GEOLOGICAL SURVEY BULLETIN 1312-O A comparison of rocks from two widely separated areas in Belt terrane UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 75-607766 4- V For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Price 35 cents CONTENTS Page Abstract .................................................................................................................. Ol Introduction ............................:.................................... .......................................... 2 General geology ...............................................................;.'................................... 3 Methods of investigation ........................y .............................................................. 7 Sampling procedure ..............................:....................................................... 7 Analytical technique for mineralogy ...............:............................................ 11 Analytical technique and calculations for geochemistry................................ 13 Mineralogy of rock types........................................................................................ 29 Geochemistry .........................................................................................................
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
Modern Mineralogy of Gold: Overview and New Data Minéralogie Moderne De L’Or : Bilan Et Nouvelles Données

ArcheoSciences Revue d'archéométrie 33 | 2009 Authentication and analysis of goldwork Modern mineralogy of gold: overview and new data Minéralogie moderne de l’or : bilan et nouvelles données Ernst Spiridonov and Denka Yanakieva Electronic version URL: http://journals.openedition.org/archeosciences/2034 DOI: 10.4000/archeosciences.2034 ISBN: 978-2-7535-1598-7 ISSN: 2104-3728 Publisher Presses universitaires de Rennes Printed version Date of publication: 31 December 2009 Number of pages: 67-73 ISBN: 978-2-7535-1181-1 ISSN: 1960-1360 Electronic reference Ernst Spiridonov and Denka Yanakieva, « Modern mineralogy of gold: overview and new data », ArcheoSciences [Online], 33 | 2009, Online since 09 December 2012, connection on 19 April 2019. URL : http://journals.openedition.org/archeosciences/2034 ; DOI : 10.4000/archeosciences.2034 Article L.111-1 du Code de la propriété intellectuelle. Modern mineralogy of gold: overview and new data Minéralogie moderne de l’or : bilan et nouvelles données Ernst Spiridonov* and Denka Yanakieva** Abstract: We suppose that it should be useful for archaeologists to have an overview on gold mineralogy, because 1) in ancient times, part of the golden objects were made directly from natural golden nuggets; 2) most of the Au in ores exists as its own minerals. he major part of the Au in the planets and meteorites of our Solar system is found in high temperature solid solutions: metallic Fe-Ni and monosulides Fe-Ni and Fe-Cu. Au leaves them under luid or some other reworking. As a result, Au minerals are formed. hey are mainly developed in hydrothermal deposits of the upper part of Earth’s continental crust.
Geochemical Analysis of Beaver River Diabase in Comparison to Anorthosite Inclusions and Similar Mid- Continental Rift Diabase

GEOCHEMICAL ANALYSIS OF BEAVER RIVER DIABASE IN COMPARISON TO ANORTHOSITE INCLUSIONS AND SIMILAR MID- CONTINENTAL RIFT DIABASE Jenna Fischer NDSU Petrology Dr. Saini- Eidukat 5/3/16 BACKGROUND MID- CONTINENT RIFT SYSTEM • Also known as Keweenawan Rift • Middle Proterozoic in age: ~ 1.1 Ga • Triple- junction rift that extends into Kansas and the lower peninsula of Michigan • Outcrops from the MRS are only seen around the Lake Superior region • Generally composed of flood basalts and intrusions • Source was a mantle plume • End of MRS could be Grenvillian orogeny (debatable) Image: www.earthscope.org Miller (1997) LAKE SUPERIOR REGION • Many intrusions in comparison to volcanic rock (60%) • Types of intrusions: Troctolitic, gabbroic, anorthositic, and granitic • Duluth Complex, North Shore Volcanic Group, and Hypabyssal Intrusions • Most hypabyssal intrusions are younger than Duluth Complex • Transitional boundary between complexes • Faults Green (1972) Miller (1997) Map: Miller and Green (2002) LAKE SUPERIOR REGION Map: Miller and Green (2002) HYPABYSSAL INTRUSIONS • Definition: a sub-volcanic rock; an intrusive igneous rock that is emplaced at medium to shallow depth within the crust between volcanic and plutonic • Largest concentration of these subvolcanic intrusions forms the Beaver Bay Complex • Whole rock compositions approximate the magma compositions • Most hypabyssal intrusions do not display igneous foliation and lack signs of differentiation • But late intrusions do! Ex. Sonju Lake, Beaver River Diabase Miller and Green (2002)
Limestone Resources of Western Washington

State of Washington DANIEL J. EVANS, Governor Department of Conservation H. MA URI CE AHLQUIST, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 52 LIMESTONE RESOURCES OF WESTERN WASHINGTON By WILBERT R. DANNER With a section on the UME MOUNTAIN DEPOSIT By GERALD W. THORSEN STATII PRINTING PLANT, OLYMPI A, WASH, 1966 For sale by Department of Conservation, Olympia, Washington. Price, $4,50 FOREWORD Since the early days of Washington's statehood, limestone has been recognized as one of the important mineral resources _of the State. The second annual report of the Washington Geological Survey, published in 1903, gave details on the State's limestone deposits, and in later years five other reports published by the Survey and its successor agencies hove given additional information on this resource. Still other reports by Federal and private agencies hove been published in response to demands for data on limestone here. Although some of the earlier reports included analyses to show the purity of the rocks, very few of the samples for analysis were taken systemati cally in a way that would fairly represent the deposits sampled. Prior to 1900 limestone was produced for use as building stone here, and another important use was for the production of burned Ii me . Portland cement plants soon became leading consumers of Ii mestone, and they con tinue as such to the present time . Limestone is used in large quantities in the pulp industry in the Northwest, and in 1966 there was one commercial lime-burning plant in the State. Recognizing the potential for industrial development in Washington based on more intensive use of our mineral resources, and recognizing the need to up-dote the State's knowledge of raw material resources in order to channel those resources into the State's growing economy, the Industrial Row Materials Advisory Committee of the Deportment of Commerce and Economic Development in 1958 recommended that a comprehensive survey be made of the limestone resources of Washington.
Structure and Petrology of the Deer Peaks Area Western North Cascades, Washington

Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Winter 1986 Structure and Petrology of the Deer Peaks Area Western North Cascades, Washington Gregory Joseph Reller Western Washington University, [email protected] Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Reller, Gregory Joseph, "Structure and Petrology of the Deer Peaks Area Western North Cascades, Washington" (1986). WWU Graduate School Collection. 726. https://cedar.wwu.edu/wwuet/726 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. STRUCTURE AMD PETROLOGY OF THE DEER PEAKS AREA iVESTERN NORTH CASCADES, WASHIMGTa^ by Gregory Joseph Re Her Accepted in Partial Completion of the Requiremerjts for the Degree Master of Science February, 1986 School Advisory Comiiattee STRUCTURE AiO PETROIDGY OF THE DEER PEAKS AREA WESTERN NORTIi CASCADES, VC'oHINGTON A Thesis Presented to The Faculty of Western Washington University In Partial Fulfillment of the requirements for the Degree Master of Science by Gregory Joseph Re Her February, 1986 ABSTRACT Dominant bedrock mits of the Deer Peaks area, nortliv/estern Washington, include the Shiaksan Metamorphic Suite, the Deer Peaks unit, the Chuckanut Fontation, the Oso volcanic rocks and the Granite Lake Stock. Rocks of the Shuksan Metainorphic Suite (SMS) exhibit a stratigraphy of meta-basalt, iron/manganese schist, and carbonaceous phyllite. Tne shear sense of stretching lineations in the SMS indicates that dioring high pressure metamorphism ttie subduction zone dipped to the northeast relative to the present position of the rocks.
Dec 15, 1999 LAB MANUAL 1209

October 2012 LAB MANUAL 1209.0 1209.0 LITHOLOGICAL SUMMARY 1209.1 GENERAL This test procedure is performed on aggregates to determine the per- centage of various rock types (especially the deleterious varieties) regulated in the Standard Specifications for Construction. 1209.2 APPARATUS A. Dilute Hydrochloric Acid (10% ±) - One part concentrated HCL with 9 parts water and eyedropper applicator B. "Brass Pencil" - (See Section 1218.2 for description) C. Balances - Shall conform to AASHTO M 231 (Classes G2 & G5). Readability & sensitivity 0.1 grams, accuracy 0.1 grams or 0.1%. Balances shall be appropriate for the specific use. D. Small Hammer, Steel Plate and Safety Glasses E. Paper Containers - Approximately 75mm (3") in diameter F. Magnifying Hand Lens (10 to 15 power) G. Unglazed Porcelain Tile (streak plate) 1209.3 TEST SAMPLE The test sample, prepared in accordance with Section 1201.4G, shall be washed (Observe washing restrictions in Section 1201.4G1c) and then dried to a constant weight at a temperature of 110 ± 5 °C (230 ± 9 °F). (See Section 1201, Table 1, for sample weights.) 1209.4 PROCEDURE Examine and classify each rock piece individually. Some rock types may need to be cracked open to identify or determine the identifying properties of the rock. (Always wear safety glasses). The following general guidelines are for informational purposes: • Always break open pieces of soft rock or any others of which you are unsure as the outside is often weathered. • Pick the easy particles first October 2012 LAB MANUAL 1209.4 • Don't be overly concerned about questionable particles unless they will fail the sample.
Papers and Proceedings of the Royal Society of Tasmania

View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Tasmania Open Access Repository ON MESOZOIC DOLERITP] AND DIABASE IN TASMANIA. By W. H. Twblvetrees, F.G.S., and W. F. Petterd, C.M.Z.S. The following Notes lay no claim to be an exhaustive description of our familiar '• diabase" or "dolerite" rock, which plays such an important part in the geology and physical configuration of our Island. The present object is rather to place upon record some inferences drawn from the examination of numerous microscopical sections of speci- mens collected or received from all parts of Tasmania. It is by accumulating the results of observations that stepping stones are formed to more complete knowledge. A glance at Mr. R. M. Johnston's geological map of Tasmania, issued by the Lands Office, will show the share this rock takes in the structure of the Island. It occupies the whole upland area of the Central Tiers. On the northern face of the Tiers—the Western Tiers as they are here called—there is a tongue of the rock prolonged northwards past IMount Claude. At their north-west corner it forms or caps mountains, such as Cradle Mountain (the highest in Tas- mania), Barn Bluff, Mount Pelion West. Eldon Blufi: forms a narrow western extension. Mount Sedgwick is a western out-lier ; Mount Dundas another. In that part of the island it is also found at Mount Heemskirk Falls, and on the Magnet Range, two miles north of the Magnet Mine. Mounts Gell and Hugel are also western out-liers.
General Index

CAL – CAL GENERAL INDEX CACOXENITE United States Prospect quarry (rhombs to 3 cm) 25:189– Not veriﬁed from pegmatites; most id as strunzite Arizona 190p 4:119, 4:121 Campbell shaft, Bisbee 24:428n Unanderra quarry 19:393c Australia California Willy Wally Gully (spherulitic) 19:401 Queensland Golden Rule mine, Tuolumne County 18:63 Queensland Mt. Isa mine 19:479 Stanislaus mine, Calaveras County 13:396h Mt. Isa mine (some scepter) 19:479 South Australia Colorado South Australia Moonta mines 19:(412) Cresson mine, Teller County (1 cm crystals; Beltana mine: smithsonite after 22:454p; Brazil some poss. melonite after) 16:234–236d,c white rhombs to 1 cm 22:452 Minas Gerais Cripple Creek, Teller County 13:395–396p,d, Wallaroo mines 19:413 Conselheiro Pena (id as acicular beraunite) 13:399 Tasmania 24:385n San Juan Mountains 10:358n Renison mine 19:384 Ireland Oregon Victoria Ft. Lismeenagh, Shenagolden, County Limer- Last Chance mine, Baker County 13:398n Flinders area 19:456 ick 20:396 Wisconsin Hunter River valley, north of Sydney (“glen- Spain Rib Mountain, Marathon County (5 mm laths donite,” poss. after ikaite) 19:368p,h Horcajo mines, Ciudad Real (rosettes; crystals in quartz) 12:95 Jindevick quarry, Warregul (oriented on cal- to 1 cm) 25:22p, 25:25 CALCIO-ANCYLITE-(Ce), -(Nd) cite) 19:199, 19:200p Kennon Head, Phillip Island 19:456 Sweden Canada Phelans Bluff, Phillip Island 19:456 Leveäniemi iron mine, Norrbotten 20:345p, Québec 20:346, 22:(48) Phillip Island 19:456 Mt. St-Hilaire (calcio-ancylite-(Ce)) 21:295– Austria United States
Oregon Geologic Digital Compilation Rules for Lithology Merge Information Entry

State of Oregon Department of Geology and Mineral Industries Vicki S. McConnell, State Geologist OREGON GEOLOGIC DIGITAL COMPILATION RULES FOR LITHOLOGY MERGE INFORMATION ENTRY G E O L O G Y F A N O D T N M I E N M E T R R A A L P I E N D D U N S O T G R E I R E S O 1937 2006 Revisions: Feburary 2, 2005 January 1, 2006 NOTICE The Oregon Department of Geology and Mineral Industries is publishing this paper because the infor- mation furthers the mission of the Department. To facilitate timely distribution of the information, this report is published as received from the authors and has not been edited to our usual standards. Oregon Department of Geology and Mineral Industries Oregon Geologic Digital Compilation Published in conformance with ORS 516.030 For copies of this publication or other information about Oregon’s geology and natural resources, contact: Nature of the Northwest Information Center 800 NE Oregon Street #5 Portland, Oregon 97232 (971) 673-1555 http://www.naturenw.org Oregon Department of Geology and Mineral Industries - Oregon Geologic Digital Compilation i RULES FOR LITHOLOGY MERGE INFORMATION ENTRY The lithology merge unit contains 5 parts, separated by periods: Major characteristic.Lithology.Layering.Crystals/Grains.Engineering Lithology Merge Unit label (Lith_Mrg_U field in GIS polygon file): major_characteristic.LITHOLOGY.Layering.Crystals/Grains.Engineering major characteristic - lower case, places the unit into a general category .LITHOLOGY - in upper case, generally the compositional/common chemical lithologic name(s)
MACROCRYSTALS of Pt–Fe ALLOY from the KONDYOR PGE PLACER DEPOSIT, KHABAROVSKIY KRAY, RUSSIA: TRACE-ELEMENT CONTENT, MINERAL INCLUSIONS and REACTION ASSEMBLAGES

601 The Canadian Mineralogist Vol. 42, pp. 601-617 (2004) MACROCRYSTALS OF Pt–Fe ALLOY FROM THE KONDYOR PGE PLACER DEPOSIT, KHABAROVSKIY KRAY, RUSSIA: TRACE-ELEMENT CONTENT, MINERAL INCLUSIONS AND REACTION ASSEMBLAGES GALINA G. SHCHEKA§ Far East Geological Institute, Russian Academy of Sciences, 159, prospect 100-letya, Vladivostok, 690022, Russia BERND LEHMANN, EIKE GIERTH AND KARSTEN GÖMANN Institute of Mineralogy and Mineral Resources, Technical University of Clausthal, Adolph-Roemer-Strasse 2a, D-38678 Clausthal-Zellerfeld, Germany ALEX WALLIANOS Max-Planck Institute of Nuclear Physics, Saupfercheckweg 1, D-69000 Heidelberg, Germany ABSTRACT Euhedral macrocrystals of Pt–Fe alloy from the Kondyor PGE placer, Khabarovskiy Kray, eastern Siberia, Russia, have a relatively constant composition of Pt2.4–2.6Fe, tin and antimony contents up to 0.3 wt.%, and an unusually low content of all PGE except Pt. The millimetric crystals contain inclusions of fluorapatite, titanite, phlogopite, magnetite, ilmenite and iron–copper sulfides. The macrocrystals have a complex gold-rich rim, with four groups of gold alloy: tetra-auricupride (the most abundant gold-bearing phase), Au–Ag (98–54 wt.% Au), Au–Ag–Cu–Pd and Au–Pd–Cu alloys. The inner part of the reaction rim hosts a variety of PGE minerals, such as stannides, antimonides and tellurobismuthides of Pd and Pt. Stannides occur as copper-bearing (taimyrite–tatyanaite series) and copper-free compounds (atokite–rustenburgite series). The main antimony mineral is Sn-bearing mertieite-II. Tellurobismuthides are represented by Te-rich sobolevskite and an intermediate member of the moncheite–insizwaite solid-solution series. The reaction rim also hosts several unknown phases, such as Pd7Bi3, Pd3Bi, Bi2O3•3H2O, and a phosphocarbonate of thorium.