Diagnostic Minerals in Metamorphosed Pelitic Rocks

Total Page:16

File Type:pdf, Size:1020Kb

Diagnostic Minerals in Metamorphosed Pelitic Rocks Diagnostic minerals in metamorphosed pelitic rocks Barrovian metamorphism — Regional orogenic metamorphism in the Scottish Highlands Chlorite zone — slates or phyllites Muscovite (important) Chlorite Biotite (higher-grade part of facies) Pyrophyllite Chloritoid Albite (lower-grade part of facies) Biotite zone — Slates give way to phyllites or schists Biotite Chlorite Muscovitee Quartz Albite Garnet zone — Schists with red almandine garnet Garnet Biotite (common) Chlorite Muscovite Quartz Albite or oligoclase Staurolite zone — Schists Staurolite Biotite Muscovite Quartz Garnet Plagioclase Chlorite (some may persist) Kyanite zone — Schists Kyanite Biotite Muscovite Quartz Plagioclase Garnet (usually) Staurolite (common) Sillimanite zone — Schists and gneisses Sillimanite Biotite Muscovite Quartz Plagioclase Garnet Staurolite (maybe) Kyanite (maybe) Minerals Diagnostic of Different Bulk Compositions in some facies of Regional Metamorphism NOTE - never are all the minerals listed for a particular bulk composition present together in a single rock. A rock contains some of the many minerals listed. This becomes clear as we consider phase diagrams which apply to metamorphic rocks of restricted composition. Quartzo-feldspathic rocks are mostly of quartz and feldspar in the greenschist, amphibolite, and pyroxene granulite facies. One or two of the minerals listed for mafic or calcareous or pelitic rocks in the appropriate facies may also be present. Symbols used: (mineral) = rare or minor constituent CAPITALIZED mineral helps distinguish rocks from next-lower-grade facies GREENSCHIST FACIES Mafic Rocks Calcareous Rocks Pelitic Rocks chlorite calcite muscovite (IMPORTANT) epidote group dolomite quartz calcite ankerite chlorite albite siderite (lower-grade GS-facies) biotite (higher-grade GS-facies) actinolite (higher-grade GS-facies) epidote group pyrophyllite (biotite) quartz chloritoid (quartz) Mg-chlorite (albite) (muscovite (lower-grade GS-facies)) (talc) Magnesian Rocks Talc; antigorite [= serpentine]; tremolite-actinolite; brucite; magnesite; chlorite EPIDOTE AMPHIBOLITE FACIES Mafic Rocks Calcareous Rocks Pelitic Rocks chlorite calcite muscovite (IMPORTANT) epidote group dolomite (but not with quartz) quartz calcite epidote group chlorite (Mg-rich) plagioclase quartz biotite (biotite) TREMOLITE ALMANDINE-spessartine (quartz) Mg-chlorite chloritoid HORNBLENDE or actinolite (plagioclase) pyrophyllite almandine-pyrope (phlogopite) (plagioclase) Magnesian Rocks Talc; antigorite [= serpentine]; tremolite-actinolite; brucite; magnesite; (chlorite) AMPHIBOLITE FACIES Mafic Rocks Calcareous Rocks Pelitic Rocks intermediate plagioclase calcite muscovite (IMPORTANT - not at high grade) hornblende dolomite (but not with quartz) quartz anthophyllite hornblende or tremolite biotite cummingtonite epidote group (low-grade A-facies) almandine epidote group (low-grade A- intermed.- or Ca-plagioclase STAUROLITE facies) almandine-pyrope diopside KYANITE or ANDALUSITE diopside forsterite (high-grade A-facies) sillimanite (high-grade A-facies) (quartz) (phlogopite ) K-feldspar-sillimanite (high-grade A-facies) (cordierite) (Mg chlorite) (low-grade A-facies) cordierite (biotite) grossularite-andradite (plagioclase) (sphene) (very-Mg-rich chlorite) (low-grade A-facies) Magnesian Rocks Anthophyllite; actinolite; olivine PYROXENE GRANULITE FACIES Mafic Rocks Calcareous Rocks Pelitic Rocks intermediate plagioclase calcite quartz AUGITE or diopside dolomite ( but not with quartz) sillimanite ENSTATITE diopside (kyanite) almandine-pyrope forsterite almandine olivine quartz orthoclase anthophyllite or cummingtonite (low-grade G- grossularite-andradite cordierite (low-grade facies) G-facies) (quartz) calcic plagioclase (plagioclase) wollastonite (high-grade G-facies) ENSTATITE Magnesian Rocks Anthophyllite or cummingtonite (low-grade G-facies); olivine; ENSTATITE BLUESCHIST FACIES Mafic Rocks Calcareous Rocks Pelitic Rocks glaucophane ARAGONITE or calcite (low-grade muscovite BS-facies) impure jadeite dolomite quartz LAWSONITE quartz stilpnomelane almandine glaucophane chlorite pumpellyite (LAWSONITE) glaucophane aragonite or calcite (low-grade BS- pumpellyite almandine facies) albite (low-grade BS-facies) chlorite (quartz) Quartzo-Feldspathic Rocks (generally derived from graywacke or arkosic arenite) Quartz; jadeite (high-grade BS-facies); LAWSONITE; glaucophane; stilpnomelane; (muscovite); albite (low-grade BS-facies); (ARAGONITE or calcite (low-grade BS-facies)) .
Recommended publications
  • CORDIERITE-GARNET GNEISS and ASSOCIATED MICRO- CLINE-RICH PEGMATITE at STURBRIDGE, I,{ASSA- CHUSETTS and UNION, CONNECTICUTI Fnor B.Cnrbn, [
    THE AMERICAN MINERALOGIST, VOL 47, IVLY AUGUST, 1962 CORDIERITE-GARNET GNEISS AND ASSOCIATED MICRO- CLINE-RICH PEGMATITE AT STURBRIDGE, I,{ASSA- CHUSETTS AND UNION, CONNECTICUTI Fnor B.cnrBn, [/. S. GeologicalSurttey, Washington,D. C. Aesrnacr Gneiss of argillaceous composition at Sturbridge, Massachusetts, and at Union, Connecticut, 10 miles to the south, consists of the assemblagebiotite-cordierite-garnet- magnetite-microcline-quartz-plagioclase-sillimanite. The conclusion is made that this assemblagedoes not violate the phase rule. The cordierite contains 32 mole per cent of Fe- end member, the biotite is aluminous and its ratio MgO: (MgOf I'eO) is 0.54, and the gar- net is alm6e5 pyr26.agro2.espe1.2.Lenses of microcline-quartz pegmatite are intimately as- sociated with the gneissl some are concordant, others cut acrossthe foliation and banding of the gneiss. The pegmatites also contain small amounts of biotite, cordierite, garnet, graphite, plagioclase, and sillimanite; each mineral is similar in optical properties to the corresponding one in the gneiss. It is suggestedthat muscovite was a former constituent of the gneiss at a lower grade of metamorphism, and that it decomposedwith increasing metamorphism, and reacted with quartz to form siliimanite in situ and at lerst part of the microcline of the gneiss and pegmatites These rocks are compared with similar rocks of Fennoscandia and Canada. INtnouucrroN Cordierite-garnet-sillimanitegneisses that contain microcline-quartz pegmatiteare found in Sturbridge,Massachusetts, and Union, Connecti- cut. The locality (Fig. 1) at Sturbridgeis on the south sideof the \{assa- chusettsTurnpike at the overpassof the New Boston Road; this is about 1 mile west of the interchangeof Route 15 with the Turnpike.
    [Show full text]
  • 17. Clay Mineralogy of Deep-Sea Sediments in the Northwestern Pacific, Dsdp, Leg 20
    17. CLAY MINERALOGY OF DEEP-SEA SEDIMENTS IN THE NORTHWESTERN PACIFIC, DSDP, LEG 20 Hakuyu Okada and Katsutoshi Tomita, Department of Geology, Kagoshima University, Kagoshima 890, Japan INTRODUCTION intensity of montmorillonite can be obtained by sub- tracting the (001) reflection intensity of chlorite from the Clay mineral study of samples collected during Leg 20 of preheating or pretreating reflection intensity at 15 Å. the Deep Sea Drilling Project in the western north Pacific In a specimen with coexisting kaolinite and chlorite, was carried out mainly by means of X-ray diffraction their overlapping reflections make it difficult to determine analyses. Emphasis was placed on determining vertical quantitatively these mineral compositions. For such speci- changes in mineral composition of sediments at each site. mens Wada's method (Wada, 1961) and heat treatment Results of the semiquantitative and quantitative deter- were adopted. minations of mineral compositions of analyzed samples are The following shows examples of the determination of shown in Tables 1, 2, 3, 5, and 7. The mineral suites some intensity ratios of reflections of clay minerals. presented here show some unusual characters as discussed below. The influence of burial diagenesis is also evidenced Case 1 in the vertical distribution of some authigenic minerals. Montmorillonite (two layers of water molecules between These results may contribute to a better understanding silicate layers)—kaolinite mixture. of deep-sea sedimentation on the northwestern Pacific This is the situation in which samples contain both plate. montmorillonite and kaolinite. The first-order basal reflec- tions of these minerals do not overlap. When the (002) ANALYTICAL PROCEDURES reflection of montmorillonite, which appears at about 7 Å, Each sample was dried in air, and X-ray diffraction is absent or negligible, the intensity ratio is easily obtained.
    [Show full text]
  • Download PDF About Minerals Sorted by Mineral Name
    MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky.
    [Show full text]
  • High Dose Dosimetry Using Antigorite-Teflon Composite
    2011 International Nuclear Atlantic Conference - INAC 2011 Belo Horizonte,MG, Brazil, October 24-28, 2011 ASSOCIAÇÃO BRASILEIRA DE ENERGIA NUCLEAR - ABEN ISBN: 978-85-99141-04-5 HIGH DOSE DOSIMETRY USING ANTIGORITE-TEFLON COMPOSITE René R. Rocca 1, Sonia H. Tatumi 2 and Shigueo Watanabe 1 1 Instituto de Física Universidade de São Paulo Rua do Matão 187 – Travessa R. 05508-090 Butantã, SP [email protected][email protected] 2 Faculdade de Tecnologia de São Paulo CEETESP Pça. Cel. Fernando Prestes - Bom retiro, 30 01124-060 São Paulo, SP [email protected] ABSTRACT Pellets of antigorite crystals (Mg 3-x [Si 2O5] (OH) 4-2x ) and teflon powder were obtained in order to investigate the thermoluminescence (TL) dosimetric characteristics. ICP analysis was performed showing the presence of 0.25 mol% of Fe 2O3, 0.07 mol% of Al 2O3 and 0.006 mol% of MnO impurities. These pellets show two prominent TL peaks at 150 oC and another broad one at 250 oC observed in samples previously irradiated with gamma-rays from 60 Co source. The 150 oC peak increased up to 2 kGy and after this dose the intensity reaches a maximum then decreases gradually. However the 250 oC peak increased up even with a dose of 172 kGy. A good reproducibility of TL results was obtained showing that these pellets can be used for high dose measurements. An excellent theoretical fit using second order kinects model [10] was obtained for all the peaks; however the theoretical deconvolution [4] showed the presence of two additional peaks at 206 and 316 oC.
    [Show full text]
  • Phase Equilibria and Thermodynamic Properties of Minerals in the Beo
    American Mineralogist, Volwne 71, pages 277-300, 1986 Phaseequilibria and thermodynamic properties of mineralsin the BeO-AlrO3-SiO2-H2O(BASH) system,with petrologicapplications Mlnx D. B.qnroN Department of Earth and SpaceSciences, University of California, Los Angeles,Los Angeles,California 90024 Ansrru,cr The phase relations and thermodynamic properties of behoite (Be(OH)r), bertrandite (BeoSirOr(OH)J, beryl (BerAlrSiuO,r),bromellite (BeO), chrysoberyl (BeAl,Oo), euclase (BeAlSiOo(OH)),and phenakite (BerSiOo)have been quantitatively evaluatedfrom a com- bination of new phase-equilibrium, solubility, calorimetric, and volumetric measurements and with data from the literature. The resulting thermodynamic model is consistentwith natural low-variance assemblagesand can be used to interpret many beryllium-mineral occurTences. Reversedhigh-pressure solid-media experimentslocated the positions of four reactions: BerAlrSiuO,,: BeAlrOo * BerSiOo+ 5SiO, (dry) 20BeAlSiOo(OH): 3BerAlrsi6or8+ TBeAlrOo+ 2BerSiOn+ l0HrO 4BeAlSiOo(OH)+ 2SiOr: BerAlrSiuO,,+ BeAlrOo+ 2H2O BerAlrSiuO,,+ 2AlrSiOs : 3BeAlrOa + 8SiO, (water saturated). Aqueous silica concentrationswere determined by reversedexperiments at I kbar for the following sevenreactions: 2BeO + H4SiO4: BerSiOo+ 2H2O 4BeO + 2HoSiOo: BeoSirO'(OH),+ 3HrO BeAlrOo* BerSiOo+ 5H4Sio4: Be3AlrSiuOr8+ loHro 3BeAlrOo+ 8H4SiO4: BerAlrSiuOrs+ 2AlrSiO5+ l6HrO 3BerSiOo+ 2AlrSiO5+ 7H4SiO4: 2BerAlrSiuOr8+ l4H2o aBeAlsioloH) + Bersio4 + 7H4sio4:2BerAlrsiuors + 14Hro 2BeAlrOo+ BerSiOo+ 3H4SiOo: 4BeAlSiOr(OH)+ 4HrO.
    [Show full text]
  • The Forsterite-Anorthite-Albite System at 5 Kb Pressure Kristen Rahilly
    The Forsterite-Anorthite-Albite System at 5 kb Pressure Kristen Rahilly Submitted to the Department of Geosciences of Smith College in partial fulfillment of the requirements for the degree of Bachelor of Arts John B. Brady, Honors Project Advisor Acknowledgements First I would like to thank my advisor John Brady, who patiently taught me all of the experimental techniques for this project. His dedication to advising me through this thesis and throughout my years at Smith has made me strive to be a better geologist. I would like to thank Tony Morse at the University of Massachusetts at Amherst for providing all of the feldspar samples and for his advice on this project. Thank you also to Michael Jercinovic over at UMass for his help with last-minute carbon coating. This project had a number of facets and I got assistance from many different departments at Smith. A big thank you to Greg Young and Dale Renfrow in the Center for Design and Fabrication for patiently helping me prepare and repair the materials needed for experiments. I’m also grateful to Dick Briggs and Judith Wopereis in the Biology Department for all of their help with the SEM and carbon coater. Also, the Engineering Department kindly lent their copy of LabView software for this project. I appreciated the advice from Mike Vollinger within the Geosciences Department as well as his dedication to driving my last three samples over to UMass to be carbon coated. The Smith Tomlinson Fund provided financial support. Finally, I need to thank my family for their support and encouragement as well as my friends here at Smith for keeping this year fun and for keeping me balanced.
    [Show full text]
  • AMPHIBOLES: Crystal Chemistry, Occurrence, and Health Issues
    AMPHIBOLES: Crystal Chemistry, Occurrence, and Health Issues 67 Reviews in Mineralogy and. Geochemistry 67 TABLE OF CONTENTS 1 Amphiboles: Crystal Chemistry Frank C. Hawthorne, Roberta Oberti INTRODUCTION 1 CHEMICAL FORMULA 1 SOMi : ASPECTS OF CHEMICAL ANALYSIS 1 Chemical composition 1 Summary 6 CALCULATION OF THE CHEMICAL FORMULA 7 24 (O, OH, F, CI) 7 23 (O) 8 13 cations 8 15 cations 8 16 cations 8 Summary 8 AMPIIIBOI I S: CRYSTAL STRUCTURE 8 Space groups 9 Cell dimensions 9 Site nomenclature 9 The C2/m amphibole structure 10 The P2/m amphibole structure 12 The P2/a amphibole structure 12 The Pnma amphibole structure 12 The Pnmn amphibole structure 14 The C1 amphibole structure 17 STACKING SEQUENCES AND SPACE GROUPS 18 BOND LENGTHS AND BOND VALENCES IN [4IA1-FREE AMPHIBOLES 19 THE DOUBLE-CHAIN OF TETRAHEDRA IN [4IA1 AMPHIBOLES 19 Variation in <T-0> bondlengths in C2/m amphiboles 21 Variation in <T-0> bondlengths in Pnma amphiboles 25 THE STEREOCHEMISTRY OF THE STRIP OF OCTAHEDRA 27 The C2/m amphiboles: variation in mean bondlengths 27 The Pnma amphiboles with B(Mg,Fe,Mn): variation in mean bondlengths 30 v Amphiboles - Table of Contents The Pnma amphiboles with BLi: variation in mean bondlengths 32 THE STEREOCHEMISTRY OF THE M (4) SITE 34 The calcic, sodic-calcic and sodic amphiboles 35 Amphiboles with small B cations (magnesium-iron-manganese- lithium, magnesium-sodium and lithium-sodium) 36 The C2/m amphiboles: variation in <M(4)-0> bondlengths 36 The Pnma amphiboles: variation in <MA-0> bondlengths 36 I III! STEREOCHEMISTRY OF THE A SITE 37 The C2/m amphiboles 37 The PU a amphibole 40 The Pnma amphiboles 40 The Pnmn amphiboles 41 THE STEREOCHEMISTRY OF THE 0(3) SITE 41 The C2/m amphiboles 41 UNIT-CELL PARAMETERS AND COMPOSITION IN C2/m AMPHIBOLES 42 SUMMARY 46 ACKNOWLEDGMENTS 46 REFERENCES 47 APPENDIX 1: CRYSTAL-STRUCTURE REFINEMENTS OF AMPHIBOLE 51 Z Classification of the Amphiboles Frank C.
    [Show full text]
  • Heat Capacity of High Pressure Minerals and Phase Equilibria of Cretan Blueschists
    Heat capacity of high pressure minerals and phase equilibria of Cretan blueschists by Matthew Rahn Manon A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology) in The University of Michigan 2008 Doctoral Committee: Professor Eric J. Essene, Chair Professor Rebecca Ann Lange Professor Youxue Zhang Associate Professor Steven M. Yalisove Matthew Rahn Manon 2008 Acknowledgments Cheers to all the grad students who have gone and come through CC-Little over the years. Zeb, Steven, Jim, Chris, Katy, Phillip, Franek, Eric, Tom, Darius, Sarah, Sara, Abir, Laura, Casey, Sam, John and anyone else I’ve been to learned something from, or argued something with. From early nights at Dominicks for subductology “seminars” through to the FWC, Michigan has been a fun place to live. Thanks to Anne Hudon, whos made sure I haven’t been able to place myself in inextricable holes. Thanks also to those from earlier in my life. College professors like Ken Hess or Barbara Nimmersheim who, in their very different ways inspired me to explore what it is I know. I’ll always remember time spent with Bob Wiebe who introduced me to the wild unknown of geology. Immeasurable thanks go to Eric Essene. The fieldtrips we took the first few years were good adventures. He’s always put aside his own issues to be there for me to talk to, especially when I didn’t deserve it. Eric’s scientific curiosity, and mental rigor are deservedly well known. His patience with me may be one of his great, unsung virtues.
    [Show full text]
  • Mineralogy, Fluid Inclusion, and Stable Isotope Studies of the Hog Heaven Mining District, Flathead County, Montana
    Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2020 MINERALOGY, FLUID INCLUSION, AND STABLE ISOTOPE STUDIES OF THE HOG HEAVEN MINING DISTRICT, FLATHEAD COUNTY, MONTANA Ian Kallio Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geological Engineering Commons MINERALOGY, FLUID INCLUSION, AND STABLE ISOTOPE STUDIES OF THE HOG HEAVEN MINING DISTRICT, FLATHEAD COUNTY, MONTANA by Ian Kallio A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Science in Geoscience Geology Option Montana Tech 2020 ii Abstract The Hog Heaven mining district in northwestern Montana is unique in that it is a high- sulfidation epithermal system containing high Ag-Pb-Zn relative to Au-Cu, with a very high Ag to Au ratio (2,330:1). The deposits are hosted within the Cenozoic Hog Heaven volcanic field (HHVF), a 30 to 36 Ma suite that consists predominantly of rhyodacite flow-dome complexes and pyroclastic rocks. The HHVF is underlain by shallow-dipping siliclastic sediments of the Mesoproterozoic Belt Supergroup. These sediments are known to host important SEDEX (e.g., Sullivan) and red-bed copper (e.g., Spar Lake, Rock Creek, Montanore) deposits rich in Ag-Pb- Zn-Cu-Ba. The HHVF erupted through and deposited on the Belt strata during a period of Oligocene extension. Outcrops and drill core samples from Hog Heaven show alteration patterns characteristic of volcanic-hosted, high-sulfidation epithermal deposits. Vuggy quartz transitions laterally into quartz-alunite alteration where large sanidine phenocrysts (up to 4 cm) have been replaced by fine-grained, pink alunite, and/or argillic alteration that is marked by an abundance of white kaolinite-dickite clay.
    [Show full text]
  • Cordierite-Bearing Gneisses in the West-Central Adirondack Highlands
    Trip A-6 CORDIERITE-BEARING GNEISSES IN THE WEST -CENTRAL ADIRONDACK HIGHLANDS Frank P. Florence Science Division, Jefferson Community College, Watertown, NY, USA 13601 [email protected] Robert S. Darling Department of Geology, SUNY College at Cortland, Cortland, NY, USA 13045 Phillip R. Whitney New York State Geological Survey (ret.), New York State Museum, Albany, NY, USA 12230 Gregory W. Lester Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, Ontario, CANADA K7L 3N6 INTRODUCTION Cordierite-bearing gneiss is uncommon in the Adirondack Highlands. To date, it is has been described from three locations, one near the village ofInlet (Seal, 1986; Whitney et aI, 2002) and two along the Moose River further to the west (Darling et aI, 2004). All of these cordierite occurrences are located in the west-central Adirondacks, a region characterized by somewhat lower metamorphic pressures as compared to the rest of the Adirondack Highlands (Florence et aI, 1995; Darling et aI, 2004). In the Fulton Chain of Lakes area of the west-central Adirondack Highlands, a heterogeneous unit of metasedimentary rocks, including cordierite-bearing gneisses, forms the core of a major NE to ENE trending synform. Cordierite appears in an assortment of mineral assemblages, including one containing the uncommon borosilicate, prismatine, the boron-rich end-member ofkornerupine (Grew et ai., 1996). The assemblage cordierite + orthopyroxene is also present, the first recognized occurrence of this mineral pair in the Adirondack Highlands (Darling et aI, 2004). This field trip includes stops at four outcrops containing cordierite in mineral assemblages that are characteristic of granulite facies metamorphism in aluminous rocks.
    [Show full text]
  • Washington State Minerals Checklist
    Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite
    [Show full text]
  • First-Principles Modeling of the Infrared Spectrum of Antigorite
    Eur. J. Mineral., 33, 389–400, 2021 https://doi.org/10.5194/ejm-33-389-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. First-principles modeling of the infrared spectrum of antigorite Etienne Balan1, Emmanuel Fritsch1,2, Guillaume Radtke1, Lorenzo Paulatto1, Farid Juillot1,2, and Sabine Petit3 1Sorbonne Université, CNRS, MNHN, Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), 4 place Jussieu, 75252 Paris CEDEX 05, France 2Institut de Recherche pour le Développement (IRD), Centre de Nouméa, 101 Promenade Roger Laroque, Anse Vata, 98848 Nouméa, New Caledonia 3Institut de Chimie des Milieux et Matériaux de Poitiers (IC2MP), CNRS UMR 7285, Université de Poitiers, 6 rue Michel Brunet, 86073, Poitiers CEDEX 9, France Correspondence: Etienne Balan ([email protected]) Received: 22 March 2021 – Revised: 14 June 2021 – Accepted: 22 June 2021 – Published: 19 July 2021 Abstract. The infrared absorption spectrum of a natural antigorite sample from New Caledonia is compared to its theoretical counterpart computed for the pristine antigorite m D 17 polysome within the density functional perturbation theory framework. The theoretical model reproduces most of the bands related to Si-O stretching −1 −1 in the 800–1300 cm range, OH libration, hindered OH translation and SiO4 bending in the 400–800 cm range, and OH stretching in the 3500–3700 cm−1 range. Most of the observed bands have a composite nature involving several vibrational modes contributing to their intensity, except the apical and one of the basal Si-O stretching bands whose intensity is carried by a single mode.
    [Show full text]