Mineraiogy, Lithostratigraphy and Geochemistry of North Lngebright Lake, Saskatchewan, Canada

Total Page:16

File Type:pdf, Size:1020Kb

Mineraiogy, Lithostratigraphy and Geochemistry of North Lngebright Lake, Saskatchewan, Canada Mineraiogy, Lithostratigraphy and Geochemistry of North lngebright Lake, Saskatchewan, Canada BY Yuqiang Shang A Thesis Submitted to the Faculty of Graduate Studies in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Department of Geological Sciences University of Manitoba Winnipeg, Manitoba (c) December, 2000 National Library Bibliothèque nationale 1+1 ,,,da du Canada Acquisitions and Acquisitions et Bibliographic Services seMces bibliographiques 395 Weliington Street 395. rue Wellington OttawaON KlAON4 Oîtawa ON KIA ON4 Canada Canada The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant a la National Library of Canada to Bhliotheque nationale du Canada de reproduce, loan, distri'bute or sell reproduire, prêter, distribuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la forme de microfiche/nlm, de reproduction sur papier ou sur format électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts from it Ni la thèse ni des extraits substantiels may be printed or otherwise de celle-ci ne doivent être imp~imés reproduced without the author's ou autrement reproduits sans son permission. autorisation. THE UNIVERSITY OF MANITOBA FACULTY OF GRADUATE STUDIES ***** COPYRIGHT PERMISSION PAGE MineraIogy, Lithostratigraphy and Geochemistry of North Iigebright Lake, Saskatchewan, Canada Yuqiang Shang A ThesidPracticum submitted to the Facuity of Graduate Studies of The University of Manitoba in partial fuif?liment of the reqnirements of the degree of Doctor of Phüosophy YUQIANG SHANG O 2000 Permission has been granted to the Library of The University of Manitoba to lend or seii copies of this thesis/practicum, to the National Library of Canada to microfilm this thesidpracticum and to lend or seii copies of the Nm, and to Dissertations Abstracts International to publish an abstract of this thesidpracticum. The author reserves other publication rights, and neither this thesidpracticum nor extensive extracts ftom it may be printed or otherwise reproduced without the author's written permission. ABSTRACT North Ingebright Lake, containing Canada's thickest known Holocene terrestrial salt sequence, is a small (1.25 km2), hypersaline playa basin located in the Great Sand HiIls area of southwestern Saskatchewan. Because of its remarkably thick lacustrine sedimentary fill, the basin offers considerable potential for providing a high resolution record of past environmental changes in a region that has few other sources of Holocene paleoenvironmental information. Until recently, efforts to acquire cores of this thick sequence of well-indurated but very soluble salt have been unsuccessful using conventional coring techniques. However, exceptional sediment recovery was achieved using a compressed-air diamond drilling technique that permitted collection of continuous, large-diameter, undisturbed and chemically unaltered cores. The 10,000 year long lacustrine sequence recovered from the basin consists of well-indurated salt, with only minor dispersed mud and organic debris. Indeed, the section is remarkable in its lack of obvious bedding, colour variation or other visible sedimentary structures. The minera1 suite of these Holocene salts consists mainly of hydrated Na, Mg, Ca, and Mg+Na sulfates, carbonates, and chlorides. Minor amounts of nitrate evaporitic minerals also occur. This long uninterrupted sequence of soluble salts implies that the lake was characterized by high salinity throughout its Holocene history. However, variations in the mineralogy of the salts suggest that the basin experienced significant changes in brÏne composition. These evaporites, which allow a detailed reconstruction of specific ion activities and ratios in the brine through time, provide our evidence of the complexity of brine evolution in a closed-basin lacustrine environment in western Canada. TABLE OF CONTENTS Abstract Paae Chapter 1 -Introduction ...................................... 1 1.1 Overview ........................................ 1 1.2 General Characteristics of Saline Lakes ............... 2 1.3 Conditions of Lake Formation in the Canadian Prairies . 4 1.4 Economic Significance of Salt Lakes ................. 6 1.5 Previous Work on North Ingebright Lake .............. 8 1.6 Objective of Research .............................. 9 1.7 Acknowledgements ............................... 10 Chapter 2 -Regional Setting ................................. 11 2.1 Physiography .................................... 11 2.2 Summary of Late Deglaciation History of the Canadian Prairies ......................................... 12 2.3StudyArea ...................................... 15 2.3.1 Location .................................. 15 2.3.2 Climate .................................. 19 2.3.3 Regional Geology .......................... 22 2.3.4 Hydrology and Hydrologie Setting .............. 25 2.4 Modern Sedimentology of North lngebright lake ....... 29 Chapter 3 -Methodology .................................... 32 3.1 Core Acquisition ................................. 32 3.1.1 Drilling Site Selection ........................ 32 3.1.2 Drilling Techniques ......................... 32 3.1.3 Diamond Drilling ........................... 36 3.1.4 Coring ................................... 38 3.2 Laboratory Analyses .............................. 40 3.2.1 Organic Matter Content ...................... 42 3.2.2 Total Carbonate Content ..................... 42 3.2.3 Chronology ...............................44 3.2.4 Mineralogy ................................ 45 3.2.5 Geochemical Simulation ..................... 46 3.2.6 Statistical Methods ......................... 48 Chapter 4 -Lithostratigraphy of North Ingebright Lake ....... 49 4.1 General Description .............................. 49 4.2 General Stratigraphic Variation of Mineralogical Constituents .................................... 57 4.3 Lithostratigraphy ................................. 60 4.3.1 Unit 1 Basal Black Mud ...................... 60 4.3.2 Unit 2 Na-Sulfate Salt ....................... 69 4.3.3 Unit 3 Mg-Carbonate--Na-Sulfate Salt ........... 70 4.3.4 Unit 4 Ca-Sulfate--Na-Sulfate Salt .............. 73 4.3.5 Unit 5 Muddy Na-Sulfate Salt ................. 75 4.3.6 Unit 6 Na-Sulfate Salt ....................... 76 4.3.7 Unit 7 Muddy Mg-Calcite--Na-Sulfate Salt ........ 77 4.3.8 Unit 8 Dolomitic Na-Sulfate Salt ............... 78 4.4 Stratigraphic Correlation Within North lngebright Lake Basin .......................................... 80 Chapter 5 -Mineralogy of North lngebright Lake Core ........ 84 5.1 General Description .............................. 84 5.2 Origin of Mineralogical Constituents ................ 84 III Significance of Carbonate Mineralogy in North lngebright Lake .................................. 86 Soluble Evaporitic Mineralogy in North lngebright Lake . 89 Chapter 6 -Geochemistry of Sedimentation ................ 108 6.1 Introduction .................................... 108 6.2 Basis of Chemical Composition Reoconstruction ..... 109 6.3 Geochemical History of North lngebright lake ........ 113 6.3.1 Unit 2 Na-Sulfate Salt ...................... 116 6.3.2 Unit 3 Mg-Carbonate--Na-Sulfate Salt .......... 119 6.3.3 Unit 4 Ca-Sulfate--Na-Sulfate Salt ............. 123 6.3.4 Unit 5 Muddy Na-Sulfate Salt ................ 124 6.3.5 Unit 6 Na-Sulfate Salt ...................... 126 6.3.6 Unit 7 Muddy Mg-Calcite--Na-Sulfate Salt ....... 128 6.3.7 Unit 8 Dolornitic Na-Sulfate Salt .............. 129 6.4 Summary of Chemical Sedimentation ............... 131 Chapter 7 -North lngebright Lake: A Dynamic Closed-Basin Lake System .................................... 134 7.1 Introduction .................................... 134 7.2 Thermodynamic Activity of H2O and Salinity ......... 134 7.3 Water Activity. Relative Humidity. and Mineral Facies . 135 7.4 Hydrological balance and Mineral Precipitation ...... 139 7.4.1 Hydrological Balance ....................... 139 7.4.2 Numerical Simulation-Mineral Precipitation ...... 142 7.5 Hydrological Conditions of North Ingebright Lake .... 153 7.6 Noth lngebright Lake Relative to Other Holocene Lacustrine Records .............................. 154 Chapter 8 -Summary . 161 References Cited . 164 Appendix A Organic Matter and Carbonate Content Data 187 Appendix B Bulk Mineralogical Data from XRD . 201 Appendix C Detailed Evaporite Mineralogy from uPDSM 273 Appendix D Major Ion Ratios of Different Çtratigraphic Units . 347 Appendix E Core Descriptions . 371 Appendix F Statistical Analyses . 374 LlST OF FIGURES . VI LlST OF TABLES . ix Figure 1.1 Classification of saline lakes . 3 Figure 2.1 Sequence of proglacial lakes in Saskatchewan and adjacent areas .................................................. 14 Figure 2.2 Map showing the sediment thickness of North lngebright Lake in the northern Great Plains of western Canada . 16 Figure 2.3 Surface deposits of the Great Sand Hills region . 20 Figure 2.4 Mean water composition (rnilli-equivalentx) of North Ingebright Lake, inflowing springs, deep groundwater and shallow groundwater . 26 Figure 2.5 Trilinear diagrams of ionic composition (milli-equivalent%) of shallow groundwater in North Ingebright Lake region . 27 Figure 2.6 Trilinear diagrams of ionic composition (rnilli-equivalent%) of de,ep groundwater in North lngebright Lake region
Recommended publications
  • 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
    [Show full text]
  • Leightonite K2ca2cu(SO4)4 • 2H2O C 2001-2005 Mineral Data Publishing, Version 1
    Leightonite K2Ca2Cu(SO4)4 • 2H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Lathlike crystals, flattened on {100}, elongated along [010], or equant, showing {100}, {101}, {110}, {113}, several other forms, to 4 mm; commonly forms cross-fiber veinlets. Twinning: On {201}. Physical Properties: Hardness = 3 D(meas.) = 2.95 D(calc.) = 2.95 Optical Properties: Transparent to translucent. Color: Pale watery blue to greenish blue; pale blue in transmitted light. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = c; Y = b; Z = a. Dispersion: r> v,moderately strong. α = 1.574–1.578 β = 1.587 γ = 1.595 2V(meas.) = ∼60◦ 2V(calc.) = 89◦060 Cell Data: Space Group: F mmm. a = 11.654(2) b = 7.497(1) c = 10.097(1) β = 125.21(1)◦ Z=2 X-ray Powder Pattern: Chuquicamata, Chile. 2.90 (100), 3.18 (60), 1.781 (30), 2.22 (20), 2.51 (10), 2.40 (10), 1.461 (10) Chemistry: (1) (2) SO3 49.33 49.87 CuO 11.97 12.39 CaO 18.41 17.46 Na2O 0.56 K2O 13.93 14.67 H2O 5.71 5.61 Total 99.91 100.00 • (1) Chuquicamata, Chile; corresponds to (K1.92Na0.12)Σ=2.04Ca2.13Cu0.98(SO4)4.00 2.06H2O. • (2) K2Ca2Cu(SO4)4 2H2O. Occurrence: Of localized occurrence in the oxidized zone of a copper deposit, probably formed under conditions of low acidity (Chuquicamata, Chile). Association: Natrochalcite, bl¨odite, atacamite, bellingerite, kr¨ohnkite,gypsum, quartz (Chuquicamata, Chile); chalcanthite, anhydrite, lammerite (Tsumeb, Namibia).
    [Show full text]
  • Lammerite Cu3(Aso4,PO4)
    Lammerite Cu3(AsO4, PO4)2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals, to 2 mm, are prismatic along [001] to tabular on {100} and terminated by {011}; additional forms include {010} and striated {120}; in radial spheroidal aggregates. Physical Properties: Cleavage: Perfect on {010}; good on {100}; imperfect on {001}. Hardness = 3.5–4 D(meas.) = 4.9–5.18 D(calc.) = 5.263 Optical Properties: Transparent. Color: Dark green. Streak: Pale green. Luster: Adamantine, vitreous on cleavage surfaces. Optical Class: Biaxial (+). Pleochroism: Strong; X = pale blue; Y = sky-blue; Z = pale bluish green. Orientation: X = b; Z ∧ c ' 40◦. Dispersion: rv, very strong. α = ∼1.89 β = 1.90–2.06 γ = 1.95–2.14 2V(meas.) = 54(5)◦ 2V(calc.) = 50◦ Cell Data: Space Group: P 21/a. a = 5.079(1) b = 11.611(2) c = 5.394(1) β = 111.72(2)◦ Z=2 X-ray Powder Pattern: Laurani, Bolivia. 2.89 (10), 2.52 (9), 3.06 (8), 3.00 (8), 2.62 (8), 2.59 (8), 2.84 (7) Chemistry: (1) (2) As2O5 49.8 32.64 P2O5 12.40 FeO 0.2 0.06 CuO 49.9 54.64 ZnO 0.8 0.11 MgO 0.2 Total 100.9 99.85 1− (1) Laurani, Bolivia; by electron microprobe, absence of (OH) and H2O confirmed by IR; corresponding to (Cu2.90Zn0.05Mg0.02Fe0.01)Σ=2.98(As1.00O4)2. (2) Tolbachik fissure volcano, Russia; by electron microprobe, corresponding to (Cu2.96Zn0.01)Σ=2.97[(As0.62P0.38)Σ=1.00O4]2.
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • Vanadium-Bearing Interlava Sediment from The
    VANADIUM-BEARING INTERLAVA SEDIMENT FROM THE CAMPBELL RIVER AREA, BRITISH COLUMBIA BY JOHN LESLIE JAMBOR B.A. University of British Columbia, 1957 THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the Department of Geology We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA April, 1960 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission-. Department of The University of British Columbia, Vancouver 3, Canada. Date CfMJ X?. ABSTRACT Vanadium is concentrated in laminated, black carbonaceous, siliceous sedimentary rocks at Menzies Bay and Quadra Island, Campbell River area, British Columbia. The vanadiferous rocks are intercalated with amygdaloidal, porphyritic basalts, andesites, and spilites, many of which are pillowform. The writer has correlated the Menzies Bay, Vancouver Island, flows with the Upper Triassic Texada formation volcanic rocks of Quadra Island. A limited petrographic study of the Texada flows in the area has indicated that pumpellyite is copious and widely distributed. Amygdaloidal greenockite is present in trace amounts. The identification of pumpellyite,re• garded as amphibole by earlier writers, marks its first occurrence in British Columbia. In a detailed study of the mineralization assoc• iated with the vanadiferous sedimentary rocks, the first British Columbian occurrences were noted for tenorite, brochantite, and cyanotrichite.
    [Show full text]
  • IMA–CNMNC Approved Mineral Symbols
    Mineralogical Magazine (2021), 85, 291–320 doi:10.1180/mgm.2021.43 Article IMA–CNMNC approved mineral symbols Laurence N. Warr* Institute of Geography and Geology, University of Greifswald, 17487 Greifswald, Germany Abstract Several text symbol lists for common rock-forming minerals have been published over the last 40 years, but no internationally agreed standard has yet been established. This contribution presents the first International Mineralogical Association (IMA) Commission on New Minerals, Nomenclature and Classification (CNMNC) approved collection of 5744 mineral name abbreviations by combining four methods of nomenclature based on the Kretz symbol approach. The collection incorporates 991 previously defined abbreviations for mineral groups and species and presents a further 4753 new symbols that cover all currently listed IMA minerals. Adopting IMA– CNMNC approved symbols is considered a necessary step in standardising abbreviations by employing a system compatible with that used for symbolising the chemical elements. Keywords: nomenclature, mineral names, symbols, abbreviations, groups, species, elements, IMA, CNMNC (Received 28 November 2020; accepted 14 May 2021; Accepted Manuscript published online: 18 May 2021; Associate Editor: Anthony R Kampf) Introduction used collection proposed by Whitney and Evans (2010). Despite the availability of recommended abbreviations for the commonly Using text symbols for abbreviating the scientific names of the studied mineral species, to date < 18% of mineral names recog- chemical elements
    [Show full text]
  • Notes, Abstracts and Reviews Are in Ordinary Type. Only Minerals for Which Definite Data Are Given Are Indexed
    TNDEX TO VOLUME 23 Leading articles are in bold face type; notes, abstracts and reviews are in ordinary type. only minerals for which definite data are given are indexed. Acmite occurrence in riebeckite- Apatite-phlogopite deposits of microgranite.(Nockold)..... l2l Quebec. (Landes). 359 Actinolite. 371 Arshinov, V. V. Pocket mineralogi- Actinolitic amphibole from New cal or polarizing magnifier.. 287 Zealand.(Hutton).... .. 539 Artz,L. C. Occurrenceof wavellite, AdelieLand rocks.(Stewart)... .. 464 GilesCo.,Va..... 664 Afirondack garnet deposits, gene- Ascharite(F). (Godlevsky)....... 294 sisof. (Miller).. ... .....174,399 Asovskite. (Efremov). 667 Ahlfeld, F. and Reyes, J. M. Aspland,V.t.... ........ 415 Mineralogie von Bolivien. Atacamite. ........706 [Book review]. 538 Atomic packing models of some Almandite. ..351.816 common sillicate structures, Aluminum and silicosis. @mmons, @orris, tr'rondel, Gtissow, Fries). 654 Lopez, Lotd, Parrish, Shimer) Alunite. jS4 ......65,182 Amalgams, natural. @ennan, Har- Austinite and brickerite, identity court).. 761 of. (Brendler) 347 Amarantite. 747 Australites, a unique shower of Aminoffite. (Hurlbut) 293 glassmeteorites. (Fenner).. 4Ls Amphibolization of sills and dikes Autunite. 275 in Libby quadrangle, Mon- Axinite,notes on. (Peacock)..... SZ2 tana.(Gibson, Jenks). ..... 3Oz Azurite. 7lO Anauxites and kaolinites, struc- tural relationshipsof .(Machat- Bandy, M. C. Mineralogy of tlree schki). tl7 sulphate deposits of Northern Andalusite in pegrnatite from Chile... 669 Fresno, Co., Calif. (Macdon- with Peacock, M. A. Un- ald, Merriam) 58S gemachite and clino-unge- Anderson,B. W... Zg3 nachite, new minerals from Anderson, C. A. Volcanoes of Chile... 314 Medicine Lake Highland, Bandylite. 704 Calif.. 166 Bandylite and a:rtofagastite, new Andradite. 432 copper minerals from Chile. Anhydrite ....... 898 (Palache, Foshag).
    [Show full text]
  • The Heteropolymolybdate Family: Structural Relations, Nomenclature Scheme and New Species
    Mineralogical Magazine, October 2012, Vol. 76(5), pp. 1175–1207 The heteropolymolybdate family: structural relations, nomenclature scheme and new species 1, 2 3 4 2 3 5 5 A. R. KAMPF *, S. J. MILLS ,M.S.RUMSEY ,M.DINI ,W.D.BIRCH ,J.SPRATT ,J.J.PLUTH ,I.M.STEELE , 6 7 R. A. JENKINS AND W. W. PINCH 1 Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA 2 Geosciences, Museum Victoria, GPO Box 666, Melbourne, Victoria 3001, Australia 3 Earth Sciences Department, Natural History Museum, Cromwell Road, London SW7 5BD, UK 4 Pasaje San Agustin 4045, La Serena, Chile 5 Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Avenue, Chicago, Illinois 60637, USA 6 4521 N. Via Madre, Tucson, Arizona 85749, USA 7 19 Stonebridge Lane, Pittsford, New York 14534, USA [Received 15 July 2012; Accepted 10 August 2012; Associate Editor: Frank Hawthorne] ABSTRACT Type specimens of the molybdoarsenates betpakdalite, natrobetpakdalite and obradovicite and the molybdophosphates mendozavilite, paramendozavilite and melkovite, and similar material from other sources, have been examined in an effort to elucidate the relations among these phases, which we designate as the heteropolymolybdate family of minerals. Using electron microprobe analysis, X-ray powder diffraction and single-crystal X-ray diffraction with crystal structure determination where possible, it was found that natrobetpakdalite, mendozavilite and melkovite are isostructural with betpakdalite and that obradovicite has a closely related structure. The betpakdalite and obradovicite structure types are based on frameworks containing four-member 3+ clusters of edge-sharing MoO6 octahedra that link by sharing corners with other clusters, with Fe O6 3+ octahedra and with PO4 or AsO4 tetrahedra (T).
    [Show full text]
  • Thn AMERICAN M INERALOGIST of AMERICA JOURNAL of the MINERALOGICAL SOCIETY
    THn AMERICAN M INERALOGIST OF AMERICA JOURNAL OF THE MINERALOGICAL SOCIETY No. 11 Vol. 23 NOVEMBER, 1938 MINERALOGY OF THREE SULPHATE DEPOSITS OF NORTHERN CHILE* Menr C. BaNov, HaraardUniaersity, Combri'd'ge, Moss' CoNrnNrs page Univer- * Based on a thesis submitted to the Division of Geological Sciences, Harvard of Philos- sity, in 1938, in partial fulfillment of the requirements for the degree of Doctor oPhY' 669 670 , MARK C. BANDV AssrRecr This paper gives the results of a study of the mineralogy of Chuquicamata, euerena, and Alcaparrosa, three sulphate deposits near calama, in Northern chile. The sulphate and chloride minerals, their description, their paragenesis, and the geochemistry of their for- mation, are the primary interest of the paper. The minerals described were collected by the author in 1935. Seventy-six minerals were identified and studied. Eighteen of these minerals are known only from northern chile and twelve are known only from these three deposits. An at- tempt has been made to clear up some of the varietal na:nes and doubtful species that have been described from these mines. Seven new well-defined mineral species were discovered during the research-antofagastite, bandylite, leightonite, ungemachite, and lindgrenite have been described elsewhere; metasideronatrite and parabutlerite are described here. For all of these. complete crystallographic, optical, and chemical data were secured. rm- portant new crystallographic data are presented for the minerals szomolnokite, pickering- ite, rhomboclase, botryogen, lapparentite and natrojarosite. New *+ay data were ob- tained on three minerals and new optical data on sixteen, and nine new chemical analyses are presented. PART I.
    [Show full text]
  • IMA/CNMNC List of Mineral Names
    IMA/CNMNC List of Mineral Name s compiled by Ernest H. Nickel & Monte C. Nichols Supplied through the courtesy of Materials Data, Inc. (http://www.MaterialsData.com) and based on the database MINERAL, which MDI makes available as a free download to the mineralogical community Status* Name CNMNC Approved Formula Strunz Classification Best, Most Recent or Most Complete reference. A Abelsonite NiC£¡H£¢N¤ 10.CA.20 American Mineralogist 63 (1978) 930 A Abenakiite-(Ce) Na¢¦Ce¦(SiO£)¦(PO¤)¦(CO£)¦(SO¢)O 9.CK.10 Canadian Mineralogist 32 (1994), 843 G Abernathyite K(UO¢)AsO¤•3H¢O 8.EB.15 American Mineralogist 41 (1956), 82 A Abhurite (SnÀÈ)¢¡Cl¡¦(OH)¡¤O¦ 3.DA.30 Canadian Mineralogist 23 (1985), 233 D Abkhazite Ca¢Mg¥Si¨O¢¢(OH)¢ 9.DE.10 American Mineralogist 63 (1978), 1023 A Abramovite Pb¢SnInBiS§ 2.HF.25a Zapiski Rossiiskogo Mineralogicheskogo Obshchetstva 136 (2007) (5), 45 D Abrazite K,Ca,Al,Si,O,H¢O 9.GC.05 Canadian Mineralogist 35 (1997), 1571 D Abriachanite Na¢(Fe,Mg)£(FeÁÈ)¢Si¨O¢¢(OH)¢ 9.DE.25 American Mineralogist 63 (1978), 1023 D Absite (U,Ca,Y,Ce)(Ti,Fe)¢O¦ Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva 92 (1963), 113 A Abswurmbachite CuÀÈ(MnÁÈ)¦O¨(SiO¤) 9.AG.05 Neues Jahrbuch für Mineralogie, Abhandlungen 163 (1991), 117 D Abukumalite (Ca,Ce)¢Y£(SiO¤,PO¤)£(O,OH,F) American Mineralogist 51 (1966), 152 D Acadialite (Ca,K,Na)(Si,Al)£O¦•3H¢O 9.GD.10 Canadian Mineralogist 35 (1997), 1571 G Acanthite Ag¢S 2.BA.30a Handbook of Mineralogy (Anthony et al.), 1 (1990), 1 A Acetamide CH£CONH¢ 10.AA.20 Zapiski Vsesoyuznogo Mineralogicheskogo
    [Show full text]
  • New Minerals from Lavrion Mining District, Greece
    New Minerals from Lavrion Mining District, Greece Authors: Branko Rieck₁, Uwe Kolitsch₂, Panagiotis Voudouris₃, Gerald Giester₄, Peter Tzeferis₅ (translated from the original “Weitere Naufunde aus Lavrion”, Griechenland, Mineralien Welt, 05/2018) Branko Rieck et al, New Minerals from Lavrion Mining District, Greece, 2018 Already shortly after the finalization of the last comprehensive description of new discoveries from the Lavrion Mining District (KOLITSCH et al. 2014) new finds were made. In parts they could be named in the article mentioned above, most however were made after the publication. It is therefore now time to open a new chapter in the description of this world- famous deposit. In the meantime, new minerals for Lavrion were found especially in polished sections and presented in a short paper for a conference (KOLITSCH et al. 2015). These and many more will be described here. In addition, an uncommon paragenesis of Uranium-bearing minerals was found in the Paleokamariza Mine #18 (SIMON & KAPELLAS 2017, RIECK 2017). And finally, there are four completely new mineral species from Lavrion currently being studied by scientists. Branko Rieck et al, New Minerals from Lavrion Mining District, Greece, 2018 All new discoveries presented here were analyzed by diffraction of X-ray on powders (PXRD) or single crystals (SXRD) and/or by semiquantitative SEM-EDS analysis. Additionally, quantitative Electron Probe and Raman Spectrometry analysis were carried out where it was deemed necessary. Branko Rieck et al, New Minerals from Lavrion Mining District, Greece, 2018 Aeschynite-(Y), (Y,Ln,Ca,Th)(Ti,Nb)2(O,OH)6 At a location discovered by the famous Greek collector Stathis Lazaridis (Lazaridisite) in the Plaka Mine #80 that is well-known for its beautiful anatase crystals in thin “alpinotype” veins also the mineral Aeschynite-(Y) could be identified.
    [Show full text]
  • MINERAL SPECIES in STOCK -- LIST 2019 This List Is an Alphabetical Listing of All Mineral Species in Stock at the Time of This Printing
    MINERALS UNLIMITED MINERAL SPECIES IN STOCK -- LIST 2019 This list is an alphabetical listing of all mineral species in stock at the time of this printing. Email or write if you need more information about any of the un-priced species. Items with an asterisk * are from the “Type” or original locality. WHAT HAS CHANGED: The 2.5cm (1”) size, as well as most other sizes shown in this list, is generally the size of the matrix, not necessarily the size of the species, with exceptions indicating (micro) with a matrix size given. Sizes with a dash (i.e. 2-3cm) indicates a range of sizes possible, and the best one will be selected from that range. If XL (or xl) is indicated, it may mean a crystal/crystal portion in the size indicated. There may be other size/price options available, ask if I haven’t listed what you want. Some species show more than one price: the higher price indicates another quality or possibly a different locality, not a larger size. Vial is 5/8-dram (about 1/2x1/2-inch area, but a smaller opening.) Where “up” follows a price, other quality specimens are available, please ask for more details. Some mineral groups have been cross-referenced, i.e., TOURMALINE, GARNET, QUARTZ, etc. For example, while the price for almandine will be found under GARNET, you will be directed to the GARNET section if you look up almandine—there you will find “Almandine—see GARNET.” Amphiboles, pyroxenes, micas, feldspars and such are listed only under their mineral names, i.e., ALBITE, BIOTITE, etc.
    [Show full text]