Mineralogical, Petrogenetic, and Geochemical Characteristics of the Meldon Aplite and Its Implications to Cornwall and Devon for Rare- Element Pegmatite Exploration

Total Page:16

File Type:pdf, Size:1020Kb

Mineralogical, Petrogenetic, and Geochemical Characteristics of the Meldon Aplite and Its Implications to Cornwall and Devon for Rare- Element Pegmatite Exploration Mineralogical, petrogenetic, and geochemical characteristics of the Meldon Aplite and its implications to Cornwall and Devon for rare- element pegmatite exploration Submitted by Janviere Uwanyirigira to the University of Exeter as a dissertation towards the degree of Master of Science in Mining geology, August, 2018. ‘I certify that the material in this dissertation which is not my own work has been identified, and that no material is included for which has been previously been conferred on me’ ………………..Signature 0 Abstract Recent development of high-tech industries and the global drive towards a carbon free economic have placed a tremendous demand on Li and placed substantial importance on exploration of lithium deposits. The Meldon Aplite has long been described as unique feature across SW England in terms of its mineralogy and exception enrichment in rare-element such as lithium, caesium, fluorine, phosphorous and niobium-tantalum. The Meldon Aplite present a potential for lithium mineralization. This study has identified a range of lithium rich minerals in the Meldon Aplite including lepidolite, elbaite, petalite, amblygonite-montebrasite, and eucryptite. It has equally ruled out the presence of spodumene in the aplite. Mineralogy and textural studies conducted in this study resulted in the identification of four different crystallization stages. These are magmatic, magmatic-hydrothermal, hydrothermal and supergene stages. In terms of lithium mineralisation, lepidolite, elbaite, petalite and amblygonite-montebrasite are primary magmatic phases with eucryptite forming at the expenses petalite complete hydrothermal replacement and clay montmorillonite forming from petalite weathering. The close association of amblygonite-montebrasite with fluorapatite indicate that it is altered at a certain extent. From trace element, the Meldon Aplite is characteristically enriched in Li (2626 to 5569 ppm), Cs (75 to 612ppm), Rb (940 to 2540 ppm), and moderately enriched in Be (8 to 84 ppm), Ta (11 to 49 ppm), and Nb (35 to 90 ppm). Such geochemistry suggest that the Meldon Aplite is relatively evolved. Comparison of Tellus (2014) soil data with the Meldon Aplite geochemistry has delineated six zones with high caesium and tantalum concentration, geochemically comparable to the Meldon Aplite. These are underlain by metasedimentary rocks, metabasic rocks and on one occasion by Gunnislake granite. The Meldon Aplite extent cannot be traced with surface exposure, however soil samples close to the aplite contain relatively elevated Rb (>62ppm). 1 Acknowledgment I wish to express my heart felt sincere gratitude to Dr Charlie Moon for providing me the opportunity to undertake this project, for his tremendous help and encouragement over the last three months. I would like to thank Ms Sharon Uren, Mr Stephen Pendray, Mr Malcolm Spence, Dr Joe Pickles and Dr Gavyn Rollinson for their help and advice with the analytical work. It is my pleasure to thank all the academic staffs at the Camborne School of Mines, University of Exeter, especially Dr Jens Andersen and Dr Robin Shail for taking their time out their busy schedule to help me with microscopy. I am grateful to the Commonwealth scholarship commission and to the University of Exeter for funding my studies. I would not end without thanking my family and friends who kept me going over the last twelve months. 2 Contents Abstract ......................................................................................................................................... 1 Chapter 1 : Introduction ................................................................................................................. 7 1.1 Introductory statement (Statement of scene of dissertation) .............................................. 7 1.2 Study Area location ............................................................................................................. 8 1.3 Aim and objectives of the project ........................................................................................ 9 1.4 Scope of the project .......................................................................................................... 10 1.4.1 Activities undertook: ....................................................................................................... 10 1.4.2 Organisation of the dissertation ..................................................................................... 10 1.4.3 Problem .......................................................................................................................... 11 1.5 Definition and Terminology ............................................................................................... 12 Chapter 2 Literature review ......................................................................................................... 13 2.1 Regional geological history of SW England ...................................................................... 13 2.1.1 Pre-Devonian basement ............................................................................................ 13 2.1.2 Rheic ocean rifting and passive margin development ............................................... 14 2.1.3 Variscan convergence and passive margin inversion ................................................ 17 2.1.4 Early post-Variscan extension ................................................................................... 19 2.1.5 Early post-Variscan tectonics and magmatism .......................................................... 20 2.1.7 Mineralization ............................................................................................................. 24 2.2 Previous work on the Meldon aplite .................................................................................. 24 2.2.1 Texture and mineralogy of Meldon aplite ................................................................... 24 2.2.2 Geographical extend of the Meldon aplite ................................................................. 27 2.3. Accounts on the occurrence and formation of rare-element pegmatites/aplites.............. 29 2.3.1 Global prospective on rare-element pegmatites/aplites ............................................. 29 2.3.2. Regional scale examination of LCT deposits ............................................................ 33 Chapter 3 Fieldwork and Sample Collection ............................................................................... 35 3.1 Field mapping .................................................................................................................... 35 3.2 Sample collection .............................................................................................................. 40 3.3 Tellus SW database .......................................................................................................... 41 Chapter 4 : Analytical Procedures .............................................................................................. 43 4.1 Sample preparation ........................................................................................................... 43 4.2 Analytical conditions .......................................................................................................... 44 Chapter 5 Results ....................................................................................................................... 46 5.1 Field aspects ..................................................................................................................... 46 5.2 Mineralogical and textural characteristics ......................................................................... 50 5.2.1 Meldon Aplite ............................................................................................................. 50 5.2.2 Summary of paragenetic diagram ....................................................................... 66 5.2.3 Host rock .................................................................................................................... 68 5.2.4 Pan concentrate ......................................................................................................... 69 5.3 Geochemical composition ................................................................................................. 69 3 5.3.1 Meldon Aplite ............................................................................................................. 69 6.3.2 Host rock .................................................................................................................... 75 5.3.3 Stream sediments ...................................................................................................... 76 5.3.3 Soil ............................................................................................................................. 76 Chapter 6 Discussion .................................................................................................................. 77 6.1 Texture, mineralogy and geochemistry of the Meldon Aplite ............................................ 77 6.1.1 Texture ....................................................................................................................... 77 6.1.2 Mineralogy .................................................................................................................. 77 6.1.3 Geochemical variation and melt evolution ................................................................. 82 6.2. Implications to the classification and petrogenesis
Recommended publications
  • Design and Discovery of New Piezoelectric Materials Using Density Functional Theory
    DESIGN AND DISCOVERY OF NEW PIEZOELECTRIC MATERIALS USING DENSITY FUNCTIONAL THEORY by Sukriti Manna © Copyright by Sukriti Manna, 2018 All Rights Reserved A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Mechanical Engineering). Golden, Colorado Date Signed: Sukriti Manna Signed: Dr. Cristian V. Ciobanu Thesis Advisor Signed: Dr. Vladan Stevanovi´c Thesis Advisor Golden, Colorado Date Signed: Dr. John Berger Professor and Head Department of Mechanical Engineering ii ABSTRACT Piezoelectric materials find applications in microelectromechanical systems (MEMS), such as surface acoustic wave (SAW) resonators, radio frequency (RF) filters, resonators, and energy harvesters. Using density functional theory calculations, the present study illus- trates the influence of alloying and co-alloying with different nitrides on piezoelectric and mechanical properties of an existing piezoelectric material such as aluminum nitride (AlN). Besides improving the performance of existing piezoelectric material, a high-throughput screening method is used to discover new piezoelectric materials. AlN has several beneficial properties such as high temperature stability, low dielectric permittivity, high hardness, large stiffness constant, high sound velocity, and complementary metal-oxide-semiconductor (CMOS) compatibility. This makes it widely accepted material in RF and resonant devices. However, it remains a challenge to enhance the piezoelectric modulus of AlN. The first part of this thesis establishes that the piezoelectric modulus of AlN could be improved by alloying with rocksalt transition metal nitrides such as scandium nitride (ScN), yttrium nitride (YN), and chromium nitride (CrN). As the content of the rocksalt end member in the alloy increases, the accompanying structural frustration enables a greater piezoelectric response.
    [Show full text]
  • 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]
  • Presentation Materials
    Annual General Meeting 25 November 2016 Creative Resources Leadership Overview § Lepidico is a well funded ASX-listed lithium exploration and development company with an experienced management team § Lepidico’s strategic objective is to become a sustainable lithium producer with a portfolio of assets and pipeline of projects § Lepidico’s exploration initiatives largely focus on hard rock minerals that prior to L-Max® were not traditional sources of lithium § Lepidico is differentiated by having successfully produced lithium carbonate and a suite of by-products from non-traditional hard rock lithium bearing minerals using its patented L-Max® process technology § Lepidico provides exposure to a portfolio of lithium exploration assets through its wholly owned properties, JV’s and IP licence agreements in Asia, Australia, Canada, Europe and South America § At 30 September 2016 Lepidico had A$3.0M in cash and no debt 2 New sources of lithium § Micas and phosphates have been largely overlooked as a source of lithium as no commercially viable process was available to extract the lithium and process through to lithium chemicals prior to L-Max® § Lithium bearing micas Lepidolite and Zinnwaldite contain up to 5% Li2O and like spodumene, are hosted in pegmatites § Lepidolite and Zinnwaldite often occur with tin and tantalum bearing minerals as well as with spodumene § Lithium phosphates such as Amblygonite contain up to 10% Li2O Lepidolite (light purple) Zinnwaldite (dArk grey) Ambygonite/MontebrAsite K(Li,Al,Rb)3(Al,Si)4O10(F,OH)2 KLiFeAl(AlSi3)O10(OH,F)2
    [Show full text]
  • Session 1 Sources and Availability of Materials for Lithium Batteries
    Session 1: Sources and Availability of Materials for Lithium Batteries Session 1 Sources and Availability of Materials for Lithium Batteries Adrian Griffin Managing Director, Lithium Australia NL ABSTRACT Lithium, as a feedstock for the battery industry, originates from two primary sources: hard-rock (generally spodumene and petalite), and brines. Brine processing results in the direct production of lithium chemicals, whereas the output from hard-rock production is tradeable mineral concentrates that require downstream processing prior to delivery, as refined chemicals, into the battery market. The processors of the concentrates, the 'converters', are the major constraint in a supply chain blessed with abundant mineral feed. The battery industry must overcome the constraints imposed by the converters, and this can be achieved through the application of the Sileach™ process, which produces lithium chemicals from concentrates direct, without the need for roasting. The cathode chemistries of the most efficient lithium batteries have a common thread – a high dependence on cobalt. Battery manufacturers consume around 40% of the current production of cobalt, a by-product of the nickel and copper industries. This means cobalt is at a tipping point – production will not keep up with demand. In the short term, the solution lies in developing alternative cathode compositions, while in the longer term recycling may be the answer. Lithium Australia NL is researching the application of its Sileach™ process to waste batteries to achieve a high-grade, low-cost source of battery materials and, in so doing, ease the supply constraints on cathode metals. To ensure that the battery industry is sustainable, better utilisation of mineral resources, more efficient processing technology, an active battery reprocessing capacity and less reliance on cobalt as a cathode material are all necessary.
    [Show full text]
  • The Challenges of Li Determination in Minerals: a Comparison of Stoichiometrically Determined Li by EPMA with Direct Measurement by LA-ICP-MS and Handheld LIBS
    The challenges of Li determination in minerals: A comparison of stoichiometrically determined Li by EPMA with direct measurement by LA-ICP-MS and handheld LIBS Robin Armstrong (NHM) THE TEAM & ACKNOWLEDGEMENTS • This work was carried out as part of the WP2 of the FAME project • The “analysts”: John Spratt & Yannick Buret (NHM) and Andrew Somers (SciAps) • The “mineralogists”: Fernando Noronha &Violeta Ramos (UP), Mario Machado Leite (LNEG), Jens Anderson, Beth Simmons & Gavyn Rollinson (CSM), Chris Stanley, Alla Dolgopolova, Reimar Seltmann & Mike Rumsey* (NHM) • Literature mineral data is taken from Mindat, Webmineral and DHZ • Robin Armstrong ([email protected]) INTRODUCTION • The analytical problems of Li • Whole Rock analysis (WR) • Examples and is it safe to make mineralogical assumptions on the base of WR • Li Mineral analysis • Li-minerals overview • Li-minerals examined • EPMA • LA-ICP-MS • LIBS • Summary and thoughts for the future LITHIUM ORES ARE POTENTIALLY COMPLEX 50mm • Li-bearing phases identified: • Lepidolite, Amblygonite-Montebrasite Li = 1.17 wt% group, Lithiophosphate(tr) and Petalite WHOLE ROCK ANALYSIS (Li ASSAYS) • Li is not that straight forward to analyse in whole rock • Its low mass means that there are low fluorescence yields and long wave-length characteristic radiation rule out lab-based XRF and pXRF • We cannot use conventional fluxes as these are generally Li- based • We can use “older” non Li fluxes such as Na2O2 but then there maybe contamination issues in the instruments • We can use multi-acid digests (HF+HNO3+HClO4 digestion with HCl-leach) (FAME used the ALS ME-MS61) however there may still be contamination issues and potentially incomplete digestion.
    [Show full text]
  • RESEARCH Petrogenesis of the Cogenetic
    RESEARCH Petrogenesis of the cogenetic Stewart pegmatite-aplite, Pala, California: Regional implications Douglas M. Morton1, J. Blue Sheppard2, Fred K. Miller3, and Cin-Ty A. Lee4 1U.S. GEOLOGICAL SURVEY AND DEPARTMENT OF EARTH SCIENCES, UNIVERSITY OF CALIFORNIA, RIVERSIDE, CALIFORNIA 92521, USA 2STEWART LITHIA MINES, P.O. BOX 382, PALA, CALIFORNIA 92059, USA 3U.S. GEOLOGICAL SURVEY, SPOKANE, WASHINGTON 99201, USA 4DEPARTMENT OF EARTH, ENVIRONMENTAL, AND PLANETARY SCIENCES, RICE UNIVERSITY, HOUSTON, TEXAS 77005, USA ABSTRACT The Stewart pegmatite-aplite dike in Pala, California (USA) is well known as a source of lithium, gem minerals, and unusual phosphate minerals. We reinterpret the petrogenesis of the dike based on a combination of new regional and detailed geochemical isotopic and textural data. The Stewart dike, like other pegmatites in the Pala district and other major pegmatite districts in the northern Peninsular Ranges batholith, is enclosed within gabbro/mafic tonalite. The 40Ar/39Ar method of dating on muscovite from the dike, and U/Pb dating of zircon from the gabbro yield essentially the same age. Initial 87Sr/86Sr is similar for the dike, 0.7042, and the gabbro, 0.7036–0.7037, indicating a juvenile and likely common source for both. The extreme mineralogic, lithologic, and textural variations within the dike are interpreted to have resulted from in situ mineral seg- regation, autometasomatism, and migration of volatiles within an essentially closed system. Contacts between the pegmatite dike and the host gabbro are diffuse. All previous interpretations of the Stewart pegmatite dike invoked an allogenic origin, formed by fluids derived externally from a nearby or distant granitic body, with the fluids subsequently migrating to, and intruding, their gabbro/mafic tonalite host.
    [Show full text]
  • Batterierohstoffe Für Lithiumionenbatterien by Dr
    DERA Industrieworkshop Lithium Batterierohstoffe für Lithiumionenbatterien by Dr. Reiner Haus Dorfner ANZAPLAN GmbH, D-92242 Hirschau, Germany www.anzaplan.com Berlin, 27. June 2017 Berlin 06-2017 page 1 © DORFNER Analysenzentrum und Anlagenplanungsgesellschaft mbH COPYRIGHT/DISCLAIMER Neither this publication nor any part thereof may be copied, reprinted, sold, published or distributed without prior written permission. This presentation provides non-binding information only and we do not assume any liability for correctness, accuracy and completeness of the information provided. Dorfner Analysenzentrum und Anlagenplanungsgesellschaft GmbH makes every effort to provide timely and accurate information. Nevertheless, mistakes and confusions may occur. The information and statistical data herein have been obtained from sources we believe to be reliable. Nevertheless, such information has not been independently verified and we do not assume any liability. Any opinions or estimates herein reflect the judgment of Dorfner Analysenzentrum und Anlagenplanungsgesell- schaft GmbH at the date of publication and are subject to changes at any time without notice. This applies especially to information reflecting estimations and technical standards since they are subject to changes over time. Dorfner Analysenzentrum und Anlagenplanungsgesellschaft GmbH does not intend, and does not assume any liability or obligation whatsoever, to update these forward-looking statements and/or estimations or to conform them to future events and developments. Berlin 06-2017 page 2 © DORFNER Analysenzentrum und Anlagenplanungsgesellschaft mbH Dorfner Group of Companies Renowned in the Industrial and Speciality Minerals Business ° Founded 1895 ° More than 100 years experience in industrial and specialty minerals processing ° Family owned ° Independent Berlin 06-2017 page 3 © DORFNER Analysenzentrum und Anlagenplanungsgesellschaft mbH Dorfner ANZAPLAN The Service Company ° Founded in 1985 to become the most independent venture within the Dorfner Group.
    [Show full text]
  • Lithium 2017
    2017 Minerals Yearbook LITHIUM [ADVANCE RELEASE] U.S. Department of the Interior September 2020 U.S. Geological Survey Lithium By Brian W. Jaskula Domestic survey data and tables were prepared by Annie Hwang, statistical assistant. In the United States, one lithium brine operation with an cobalt oxide and 2,160 kg of lithium-nickel-cobalt-aluminum associated lithium carbonate plant operated in Silver Peak, oxide (Defense Logistics Agency Strategic Materials, 2017). At NV. Domestic and imported lithium carbonate, lithium yearend 2017, the NDS held 540 kg of lithium-cobalt oxide and chloride, and lithium hydroxide were consumed directly 1,620 kg of lithium-nickel-cobalt-aluminum oxide. in industrial applications and used as raw materials for downstream lithium compounds. In 2017, lithium consumption Production in the United States was estimated to be equivalent to The U.S. Geological Survey (USGS) collected domestic 3,000 metric tons (t) of elemental lithium (table 1) [16,000 t production data for lithium from a voluntary canvass of the of lithium carbonate equivalent (LCE)], primarily owing to only U.S. lithium carbonate producer, Rockwood Lithium Inc. demand for lithium-based battery, ceramic and glass, grease, (a subsidiary of Albemarle Corp. of Charlotte, NC). Production pharmaceutical, and polymer products. In 2017, the gross weight and stock data collected from Rockwood Lithium were withheld of lithium compounds imported into the United States increased from publication to avoid disclosing company proprietary data. by 7% and the gross weight of exports increased by 29% from The company’s 6,000-metric-ton-per-year (t/yr) Silver Peak those in 2016.
    [Show full text]
  • Extraction of Zinnwaldite from Mining and Processing Wastes
    Sborník vědeckých prací Vysoké školy báňské – Technické univerzity Ostrava Řada hornicko-geologická Volume LI (2005), No.2, p. 9-16, ISSN 0474-8476 Jiří BOTULA*, Pavel RUCKÝ**, Vlastimil ŘEPKA*** EXTRACTION OF ZINNWALDITE FROM MINING AND PROCESSING WASTES ZÍSKÁVÁNÍ CINVALDITU Z ODPADŮ PO TĚŽBĚ A ÚPRAVĚ Abstract Lithium is the lightest metal in the periodic table of elements, whose world reserves in the available deposits are estimated to be 20Mt, and in the Czech Republic Li makes up about 1% of the world reserves as the residual element in Sn-W ore mineralization. Significant reserves of Li are also represented in waste from the former mining and processing of Sn-W ores in the Krušné hory region, containing about 0.2% Li. The world consumption of lithium is estimated 6 kt/year and a gradual increase is expected, as well as an increase of the price. With regard to the fact that the consumption of Li in the Czech Republic is covered by the import, it would be suitable to eliminate this dependence to some extent and utilize the Czech resources of Li for production. At the beginning, the easiest method seems to be utilization of the present waste piles from the gravity processing of Sn-W ores in the estimated amount of 3.5 Mt in the former deposit of Cínovec. This paper is devoted to the possibilities of extracting Li-concentrates from raw materials. Abstrakt Lithium je nejlehčím kovem periodické soustavy prvků, jehož světové zásoby v dostupných ložiscích se odhadují na 20Mt, přičemž v České republice tvoří Li jako doprovodný prvek Sn-W zrudnění přibližně 1% světových zásob.
    [Show full text]
  • Crimsonite, Pbfe23+(PO4)
    Mineralogical Magazine, October 2016, Vol. 80(6), pp. 925–935 3+ Crimsonite, PbFe2 (PO4)2(OH)2, the phosphate analogue of carminite from the Silver Coin mine, Valmy, Nevada, USA 1,* 2 3 4 A. R. KAMPF ,P.M.ADAMS ,S.J.MILLS AND B. P. NASH 1 Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA 2 126 South Helberta Avenue #2, Redondo Beach, California 90277, USA 3 Geosciences, Museum Victoria, GPO Box 666, Melbourne 3001, Victoria, Australia 4 Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112, USA [Received 28 May 2015; Accepted 10 September 2015; Associate Editor: Ian Graham] ABSTRACT 3þ Crimsonite (IMA2014-095), PbFe2 (PO4)2(OH)2, the phosphate analogue of carminite, is a new mineral from the Silver Coin mine, Valmy, Iron Point district, Humboldt County, Nevada, USA, where it occurs as a low-temperature secondary mineral in association with fluorwavellite, goethite, hematite, hentschelite, plumbogummite and variscite on quartz. Crimsonite occurs in subparallel aggregates of deep red blades or plates flattened on {100} and up to 0.1 mm in maximum dimension. The streak is light purplish orange. Crystals are transparent and have adamantine lustre. The Mohs hardness is ∼3½, the tenacity is brittle, the fracture is irregular to splintery and an imperfect cleavage is likely on {101}. The calculated density is 5.180 g/cm3. Crimsonite is optically biaxial (+), with 2V = 85.5(5)° and γ – α = 0.011. Using the Gladstone- Dale relationship, the calculated indices of refraction are α = 2.021, β = 2.026 and γ = 2.032.
    [Show full text]
  • A Review of Lithium Occurrences in Africa
    A Review of Lithium occurrences in Africa Paul Nex, Kathryn Goodenough, Richard Shaw and Judith Kinnaird Lithium occurrences and exploration activity in Africa are dominated by pegmatite occurrences . Greenbushes, Australia No known brine resources as yet, Mineral Formula although Spodumene LiAl(SiO3)2 Botswana is Petalite LiAlSi4O10 being Eucryptite LiAlSiO4 investigated: Amblygonite (Li,Na)AlPO (F,OH) (by Lithium 4 Consolidated Mineral Lepidolite K(Li,Al)3(Al,Si,Rb)4O10(F,OH) Exploration Ltd-ASX) Pegmatites:typically granitic, enriched in incompatible elements, occurrences correlate with times of collisional orogeny and supercontinent assembly. Pegmatite classification needs reworking, however two types of interest - LCT: Lithium-caesium-tantalum NYF: Niobium-yttrium-fluorine Rubicon (Namibia) Bikita (Zimbabwe) Two dominant genetic models: 1. Products of the fractionation of a parental granite. 2. Products of low volume partial melting of metasediments during post-collisional orogenic collapse associated with decompression Nigeria: Pegmatites are ~probably younger than 560 Ma. Contenders for parental granites are 640-600 Ma Recent research in Norway (Muller et al 2017, or 60-580 Ma “thousands of pegmatites without parental granites”), NW Scotland, Nigeria and Namibia suggests that the low volume partial melting model for the genesis of granitic pegmatites is more prevalent than previously appreciated. In Namibia, potential parental granites are ~25 Ma older than the pegmatites and are deformed while the pegmatites are undeformed Most
    [Show full text]
  • ~Ui&£R5itt! of J\Rij!Oua
    Minerals and metals of increasing interest, rare and radioactive minerals Authors Moore, R.T. Rights Arizona Geological Survey. All rights reserved. Download date 06/10/2021 17:57:35 Link to Item http://hdl.handle.net/10150/629904 Vol. XXIV, No.4 October, 1953 ~ui&£r5itt! of J\rij!oua ~ul1etiu ARIZONA BUREAU OF MINES MINERALS AND METALS OF INCREASING INTEREST RARE AND RADIOACTIVE MINERALS By RICHARD T. MOORE ARIZONA BUREAU OF MINES MINERAL TECHNOLOGY SERIES No. 47 BULLETIN No. 163 THIRTY CENTS (Free to Residents of Arizona) PUBLISHED BY ~tti£ll~r5itt! of ~rh!Omt TUCSON, ARIZONA TABLE OF CONTENTS INTRODUCTION 5 Acknowledgments 5 General Features 5 BERYLLIUM 7 General Features 7 Beryllium Minerals 7 Beryl 7 Phenacite 8 Gadolinite 8 Helvite 8 Occurrence 8 Prices and Possible Buyers ,........................................ 8 LITHIUM 9 General Features 9 Lithium Minerals 9 Amblygonite 9 Spodumene 10 Lepidolite 10 Triphylite 10 Zinnwaldite 10 Occurrence 10 Prices and Possible Buyers 10 CESIUM AND RUBIDIUM 11 General Features 11 Cesium and Rubidium Minerals 11 Pollucite ..................•.........................................................................., 11 Occurrence 12 Prices and Producers 12 TITANIUM 12 General Features 12 Titanium Minerals 13 Rutile 13 Ilmenite 13 Sphene 13 Occurrence 13 Prices and Buyers 14 GALLIUM, GERMANIUM, INDIUM, AND THALLIUM 14 General Features 14 Gallium, Germanium, Indium and Thallium Minerals 15 Germanite 15 Lorandite 15 Hutchinsonite : 15 Vrbaite 15 Occurrence 15 Prices and Producers ~ 16 RHENIUM 16
    [Show full text]