Mineralogy and Geology of the \Vkgnerite Occurrence Co Santa Fe Mountain, Front Range, Cobrado

Total Page:16

File Type:pdf, Size:1020Kb

Mineralogy and Geology of the \Vkgnerite Occurrence Co Santa Fe Mountain, Front Range, Cobrado Mineralogy and Geology of the \Vkgnerite Occurrence co Santa Fe Mountain, Front Range, Cobrado GEOLOGICAL SURVEY PROFESSIONAL PAPER 955 Mineralogy and Geology of the Wignerite Occurance on Santa Fe Mountain, Front Range, Colorado By DOUGLAS M. SHERIDAN, SHERMAN P. MARSH, MARY E. MROSE, and RICHARD B. TAYLOR GEOLOGICAL SURVEY PROFESSIONAL PAPER 955 A detailed mineralogic study of wagnerite, a rare phosphate mineral occurring in the report area in Precambrian gneiss; this is the first recorded occurrence of wagnerite in the United States UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main entry under title: Mineralogy and geology of the wagnerite occurrence on Santa Fe Mountain, Front Range, Colorado. (Geological Survey Professional Paper 955) Includes bibliographical references. 1. Wagnerite Colorado Santa Fe Mountain. 2. Geology Colorado Santa Fe Mountain. I. Sheridan, Douglas M., 1921- II. Series: United States Geological Survey Professional Paper 955. QE391.W3M56 549'.72 76-10335 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, B.C. 20402 Stock Number 024-001-02844-1 CONTENTS Page Metric-English equivalents .............................. Descriptive mineralogy Continued Page Abstract............................................................ 1 Wagnerite............................................... 5 Introduction..................................................... 1 Other minerals....................................... 8 Acknowledgments............................................ 2 Mineral assemblages and textural relations. 11 Geologic setting............................................... 2 Chemistry...................................................... 14 Occurrence....................................................... 3 X-ray crystallography................................... 15 Descriptive mineralogy.................................... 5 Origin............................................................ 19 Methods used for optical determinations. 5 References cited............................................. 22 ILLUSTRATIONS Page FIGURE 1. Map of east-central Front Range showing Santa Fe Mountain wagnerite locality and location of figure 2.................................. 2 2. Map showing distribution of rutile-bearing light-colored gneisses in the Santa Fe Mountain-Beaver Brook-Soda Creek area ...................................................................................................................................................................................^ 3 3. Geologic map of wagnerite locality, Santa Fe Mountain ................................................................................................................. 4 Photomicrographs: 4. Large ameboid-shaped grain of wagnerite...................................................................................................................... 6 5. Large blocky grain of wagnerite poikiloblastically enclosing rows of rutile grains..................................................... 7 6. Complex intergrowth of closely spaced grains of wagnerite and plagioclase............................................................... 7 7. Part of a large wagnerite grain that is crowded with tiny inclusions ........................................................................... 8 8, 9. Rims of apatite on wagnerite.......................................................................................................................................... 8, 9 10. Prismatic to blocky inclusions of apatite in wagnerite.................................................................................................. 9 11, 12. Wagnerite strongly oriented parallel to foliation defined by fibrolitk sillimanite....................................................... 11, 12 13, 14. Prismatic sillimanite cutting wagnerite and other minerals.......................................................................................... 12, 13 15. Corundum containing numerous needles of sillimanite................................................................................................ 13 16. Corundum and rutile along grain boundaries of wagnerite.......................................................................................... 13 17. X-ray powder photographs of wagnerite, ferroan wagnerite, magniotriplite, and triplite........................................... 20 TABLES Page TABLE 1. Modes of light-colored gneisses, Santa Fe Mountain wagnerite locality, Colorado......................................................................... 5 2. Optical data for wagnerite from Santa Fe Mountain, Colorado....................................................................................................... 5 3. Comparison of optical data for wagnerite......................................................................................................................................... 5 4. Optical data for other minerals from wagnerite locality, Santa Fe Mountain, Colorado................................................................ 10 5. Chemical analyses of wagnerite ......................................................................................................................................................... 14 6. Microprobe analysis of wagnerite from Santa Fe Mountain, Colorado............................................................................................ 15 7. Crystallographic, compositional, and density data compared for wagnerite, ferroan wagnerite, magniotriplite, and triplite......................................................................................................................................................... ig 8. X-ray powder diffraction data for wagnerite, Mg2(PO4)F................................................................................................................. 17 III IV CONTENTS METRIC-ENGLISH EQUIVALENTS Metric unit English equivalent Metric unit English equivalent Length Specific combinations Continued millimetre (mm) = 0.03937 inch (in) litre per second (1/s) = .0353 cubic foot per second metre (m) = 3.28 feet (ft) cubic metre per second kilometre (km) = .62 mile (mi) per square kilometre [(m»/s)/km2] Area square mile [(fts/s)/rni2] metre per day (m/d) = 3.28 feet per day (hydraulic square metre (m2) = 10.76 square feet (ft2) conductivity) (ft/d) square kilometre (km2) = .386 square mile (mi2) metre per kilometre hectare (ha) = 2.47 acres (m/km) = 5.28 feet per mile (ft/mi) kilometre per hour (km/h) = .9113 foot per second (ft/s) Volume metre per second (m/s) 3.28 feet per second cubic centimetre (cm3) = 0.061 cubic inch (in3 ) metre squared per day litre (1) = 61.03 cubic inches (m2/d) = 10.764 feet squared per day (ft2/d) cubic metre (m3) = 35.31 cubic feet (ft3) (transmissivity) cubic metre = .00081 acre-foot (acre-ft) cubic metre per second cubic hectometre (hm3 = 810.7 acre-feet (mVs) = 22.826 million gallons per day litre = 2.113 pints (pt) (Mgal/d) litre = 1.06 quarts (qt) cubic metre per minute litre = .26 gallon (gal) (rn3/min) = 264.2 gallons per minute (gal/min) cubic metre = .00026 million gallons (Mgal or litre per second (1/s) = 15.85 gallons per minute 10« gal) litre per second per cubic metre = 6.290 barrels (bbl) (1 bbl = 42 gal) metre [(l/s)/m] = 4.83 gallons per minute per foot [( gal/min) /ft] kilometre per hour Weight (km/h) .62 mile per hour (mi/h) gram (g) = 0.035 ounce, avoirdupois (oz sivdp) metre per second (m/s) = 2.237 miles per hour gram = .0022 pound, avoirdupois (Ib avdp) gram per cubic tonne (t) = 1.1 tons, short (2,000 Ib) centimetre (g/crn3) = 62.43 pounds per cubic foot (lb/fts) tonne = .98 ton, long (2,240 Ib) gram per square centimetre (g/cm2) 2.04S pounds per square foot (lb/ft2) gram per square Specific combinations centimetre .0142 pound per square inch (lb/in2) kilogram per square centimetre (kg/cm2) = 0.96 atmosphere (atm) Temperature kilogram per square centimetre = .98 bar (0.9869 atm) degree Celsius (°C) = 1.8 degrees Fahrenheit (°P) cubic metre per second degrees Celsius (mVs) = 35.3 cubic feet per second (ft3/s) (temperature) = [(l.SX°C)+32] degrees Fahrenheit MINERALOGY AND GEOLOGY OF THE WAGNERITE OCCURRENCE ON SANTA FE MOUNTAIN, FRONT RANGE, COLORADO By DOUGLAS M. SHERIDAN, SHERMAN P. MARSH, MARY E. MROSE, and RICHARD B. TAYLOR ABSTRACT magniotriplite; this material should not be referred to as ferroan The first known occurrence in the United States of wagnerite, a rare wagnerite. Although X-ray powder-diffraction patterns of ferroan magnesium fluophasphate, is on Santa Fe Mountain near Idaho Springs wagnerite and magniotriplite resemble the diffraction pattern of in the Colorado Front Range. Wagnerite occurs as a minor constituent of wagnerite, the pattern for wagnerite has a line at 5.66 A which thin lenses of sillimanite-plagioclase gneiss of Precambrian age. Other distinguishes it from triplite-group minerals. minerals in the gneiss are corundum, rutile, pale-brown biotite, apatite, Rutile-bearing gneisses in the east-central Front Range are believed to monazite, zircon, and tourmaline. The sillimanite-plagioclase gneiss is a have formed by metamorphism of bentonitic clays that were generated local lithologic variant of a persistent layer of rutile-bearing sillimanite- during intense weathering of intermediate to basic
Recommended publications
  • The Krásno Sn-W Ore District Near Horní Slavkov: Mining History, Geological and Mineralogical Characteristics
    Journal of the Czech Geological Society 51/12(2006) 3 The Krásno Sn-W ore district near Horní Slavkov: mining history, geological and mineralogical characteristics Sn-W rudní revír Krásno u Horního Slavkova historie tìby, geologická a mineralogická charakteristika (47 figs, 1 tab) PAVEL BERAN1 JIØÍ SEJKORA2 1 Regional Museum Sokolov, Zámecká 1, Sokolov, CZ-356 00, Czech Republic 2 Department of Mineralogy and Petrology, National Museum, Václavské nám. 68, Prague 1, CZ-115 79, Czech Republic The tin-tungsten Krásno ore district near Horní Slavkov (Slavkovský les area, western Bohemia) belongs to the most important areas of ancient mining in the Czech Republic. The exceptionally rich and variable mineral associations, and the high number of mineral species, make this area one of the most remarkable mineralogical localities on a worldwide scale. The present paper reviews the data on geological setting of the ore district, individual ore deposits and mining history. Horní Slavkov and Krásno were known as a rich source of exquisite quality mineral specimens stored in numerous museum collections throughout Europe. The old museum specimens are often known under the German locality names of Schlaggenwald (= Horní Slavkov) and Schönfeld (=Krásno). The megascopic properties and paragenetic position of selected mineral classics are reviewed which include arsenopyrite, fluorapatite, fluorite, hübnerite, chalcopyrite, carpholite, cassiterite, quartz, molybdenite, rhodochrosite, sphalerite, topaz and scheelite. Key words: Sn-W ores; tin-tungsten mineralization; mining history; ore geology; mineralogy; Slavkovský les; Krásno, Horní Slavkov ore district; Czech Republic. Introduction valleys dissected parts of the area. In the ore district area, the detailed surface morphology is modified by large de- In the mining history of Central Europe, Bohemia and pressions caused by the collapse of old underground Moravia are known as important source of gold, silver, workings and by extensive dumps.
    [Show full text]
  • 1 CRYSTAL CHEMISTRY of SELECTED Sb, As and P MINERALS
    Crystal Chemistry of Selected Sb, As, and P Minerals Item Type text; Electronic Dissertation Authors Origlieri, Marcus Jason Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 10:49:41 Link to Item http://hdl.handle.net/10150/194240 1 CRYSTAL CHEMISTRY OF SELECTED Sb, As AND P MINERALS by Marcus Jason Origlieri ___________________________________________ A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 2005 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Dissertation Committee, we certify that we have read the dissertation prepared by Marcus Jason Origlieri entitled Crystal Chemistry of Selected Sb, As, and P Minerals and recommend that it be accepted as fulfilling the dissertation requirement for the Degree of Doctor of Philosophy _______________________________________________________________________ Date: November 15, 2005 Robert T. Downs _______________________________________________________________________ Date: November 15, 2005 M. Bonner Denton _______________________________________________________________________ Date: November 15, 2005 Mihai N. Ducea _______________________________________________________________________ Date: November 15, 2005 Charles T. Prewitt Final approval and acceptance of this dissertation is contingent upon the candidate’s submission of the final copies of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement.
    [Show full text]
  • LAB 3: COMMON MINERALS in SEDIMENTARY ROCKS, Part 1
    EESC 2100: Mineralogy LAB 3: COMMON MINERALS IN SEDIMENTARY ROCKS, Part 1 Learning Objectives: Students will be able to identify minerals that occur commonly in sandstones (quartz and feldspars), both in hand-sample and thin-section Students will be able to determine the composition of plagioclase using the Michel-Levy method New Minerals: Quartz, Plagioclase, Microcline, Orthoclase Clastic sedimentary rocks are composed of grains that have been weathered from pre-existing rocks. The chemical weathering processes of hydrolysis, oxidation, and dissolution act on sediments, destroying those minerals that are most reactive, and forming new minerals that are stable at surface conditions: most halides and sulfates will dissolve; pyrite will form hydroxy-oxides such as limonite; unstable silicates will form clays. Minerals that are susceptible to physical weathering (i.e., minerals that are soft or cleavable) will be reduced in size during transport, and so may only be identified under the microscope. Quartz is a common rock-forming mineral, and resistant to both chemical and physical weathering. Accordingly, it is a common constituent of clastic sedimentary rocks. Feldspars are relatively stable in the surface environment, with potassium feldspars being more resistant to chemical weathering than plagioclase. Mafic minerals readily weather to form clays and iron hydroxy- oxides, and so are uncommon in sedimentary rocks. Thus the most important minerals in clastic sedimentary rocks are quartz, potassium feldspar (microcline and orthoclase), plagioclase, clays, and oxides/hydroxy-oxides (hematite, limonite, goethite). Percentages of quartz, feldspar, and clay are used to classify most clastic sedimentary rocks (sandstones, siltstones, claystones). QUARTZ Examine the four hand samples of quartz (Crystal, White, var.
    [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]
  • Phosphates, Arsenates, Vanadates, Antimonates A
    592 DESCRIPTIVE MINERALOGY Epistdite. A niobate of uncertain composition. Analysis shows chiefly SjOz, TiOz, NkO, H20. Monoclinic. In rectangular plates, also in aggregates of curved foha. Basal cleavage perfect. H. = 1-1.5. G. = 2.9. Color white, grayish brownish. Refractive index 1.67. Bound in pegmatite veins or in massive albite from ~llianehaab,Greenland. Plumboniobite. A niobatc of yttrium, uranium, lead, iron, etc. Amorphous. H. = 5-5'5. G. = 4.81. Color dark brown to black. Found in mica mines at Morogoro, German Enst Africa. Oxygen Salts 4. PHOSPHATES, ARSENATES, VANADATES, ANTIMONATES A. Anhydrous Phosphates, Arsenates, Vanadates, Antimonates Normal phosphoric acid is H3P04, and consequently normal phosphates I 11 m have the formulas RtPOa, R3(PO4)2 and RPO4, and similarly for the arse- nates, etc. Only a comparatively small number of species conform to this simple formula. Most species contain more than one metallic element, and in the prominent Apatite Group the radical (CaF), (CaCI) or (PbCI) enters; " in the Wagnerite Group we have similarly (kF) or (ROH). XENOTIME. Tetragonal. Axis c = 0.6187, zz' (1 11 A ill) = 55" 301, 22" (111 A 771) = 82" 22'. In crystals resembling zircon in habit; sometimes compounded with zircon in parallel position (Fig. 462, p. 173). In 972 rolled grains. Cleavage: m (110) perfect. Fracture uneven and splintery. Brittle. H. = 4-5. G. = 4.454.56. Luster resinous to vitreous. Color yellowish brown, reddish brown, hair-brown, flesh-red, grayish white, wine-yellow, pale yellow; streak pale brown, yellow- ish or reddish. Opaque. Optically + . w = 1.72. e = 1-81.
    [Show full text]
  • NEW MINERALS It Is Proposed Hereafter to Indicate In.A General Way the Classification of All New Minerals Recoided in This Department
    JOURNAL MINERALOGICAL SOCIETY OF AMENICA 63 Dr. Kunz then spoke of the various city localities and the minerals found therein. He stated that the East Side, from 37 to 110 St., probably afforded the most specimens. The various tunnels and their minerals were spoken of. Capt. Miller called attention to the fine collection of Brooklyn Drift Minerals and Rocks in the collection of the Long Island Historical Society. Ife abo mentioned the occurrence of monazite and xenotime crystals, on the Speedway,Harlem River. Dr. Kunz emphasizedthe irnportance of complete records being kept of all finds. Tnou,q,s L Mrr,r,nn, SecretaryPro, Tem. NEW MINERALS It is proposed hereafter to indicate in.a general way the classification of all new minerals recoided in this department. Subdivision will be first into "families," of which nine may be recognized,as listed in the January number (Am. Min.6 (1), 12,1921). Eachfamilywillbe separatedinto "subfamilies " based on special features of composition. This arrangement is tentative and open to modification, and criticism of it will be welcome, [Eo.] FAMILY 2. SULFIDES, ETC. SosreMrr,v 3. Doust,u suLFrDEs oF METALSAND sEMr-METAr,s. I'LTRABASITE V. Rosrcxf and J. Srnnse-Btinu. Ultrabasit, ein neues Mineral aus Freiberg in Sachsen. (Ultrabasite, a new mineral from Freiberg, Saxony). Rozpr.Eeslcd Ako,il. Prag,25, No. 45, 1916;Z. Krgst. Min., 55,43H39, 1920, Neun: From its extremely basic chemical composition. Pnrsrcar, Pnopnnrrus Color black, somewhat grayish; luster metallic; streak black; cleavage none; fracture scaly, with somewhat greasy luster on the surface. H. : 5; sp. gr.
    [Show full text]
  • Download the Scanned
    164 THE AMERICAN MINERAI,OGIST TABLE 3 Tlaln ro ssow Mnrnoo or Cer,cur,rfioN oF Axer,ns (SeeWi,nkeltabellen, pp. 18, 19 & 19a). Mlneral Etggttrslte Elements Do:1.272 I€t, Symb, lg Po: 010449 pq qo: .7940 lcp lgq lc so:989982 o I 0 0 01044e oaoosz I p+I 969897 0 e80346 e8es82 I 2 017609 030103 028058nrF,osR I 020085O200R5 qqo :te lpo p lg@:lgtanp lgsin 9 lg cos 9 I sn @ owQ qqo :19 tan p lrom 8 lrom 8 trcm 5 lrom I 3-6:4-7 020467 992858 972381 5802', 017591 56018', 017601 990364 979605 989233 38 42 000741 45 30 000749 007973 988573 980595 50 14 039485 68 04 039490 LISTS OF THE ORTIIORIIOMBIC MINERALS INCLUDED IN GOLDSCIIMIDT'S WINKELTABELLEN. Eocen T. WEONNY. WASh. ington, D. C.-As the prism zone is on the whole most cha.racteristicof orthor- hombic crystals, it has seemeddesirable to arrange the minerals of this system in the order of increasins values of axis a, Onrsonsolmrc MTNERALS ac Page a c Page Uranophanite......0.311.01 355 Tooaz. .....0.53 0.95 346 Polycrasite (Poly- Puiherite..........0.53l.l7 274 kras)...........0.35 0.31 27r Phosohosiderite....0.53 0.88 266 Euxenite ...0.36 0.30 r37 .Iordinite ...0.54 l.oz 191 Molybdite....:....0.39 0,47 243 Yttrobantalite......0.54 1.13 371 Columbite ..0.40 0.36 101 Rammelsbergite....0.54 - 291 Oanneroedite (An- Samarskite.........0.550.52 309 ner<idit).........0.400.36 45 Struvite ....0.55 0.62 332 Flinkite .
    [Show full text]
  • New Mineral Names*,†
    American Mineralogist, Volume 106, pages 1360–1364, 2021 New Mineral Names*,† Dmitriy I. Belakovskiy1, and Yulia Uvarova2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2CSIRO Mineral Resources, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia In this issue This New Mineral Names has entries for 11 new species, including 7 minerals of jahnsite group: jahnsite- (NaMnMg), jahnsite-(NaMnMn), jahnsite-(CaMnZn), jahnsite-(MnMnFe), jahnsite-(MnMnMg), jahnsite- (MnMnZn), and whiteite-(MnMnMg); lasnierite, manganflurlite (with a new data for flurlite), tewite, and wumuite. Lasnierite* the LA-ICP-MS analysis, but their concentrations were below detec- B. Rondeau, B. Devouard, D. Jacob, P. Roussel, N. Stephant, C. Boulet, tion limits. The empirical formula is (Ca0.59Sr0.37)Ʃ0.96(Mg1.42Fe0.54)Ʃ1.96 V. Mollé, M. Corre, E. Fritsch, C. Ferraris, and G.C. Parodi (2019) Al0.87(P2.99Si0.01)Ʃ3.00(O11.41F0.59)Ʃ12 based on 12 (O+F) pfu. The strongest lines of the calculated powder X-ray diffraction pattern are [dcalc Å (I%calc; Lasnierite, (Ca,Sr)(Mg,Fe)2Al(PO4)3, a new phosphate accompany- ing lazulite from Mt. Ibity, Madagascar: an example of structural hkl)]: 4.421 (83; 040), 3.802 (63, 131), 3.706 (100; 022), 3.305 (99; 141), characterization from dynamic refinement of precession electron 2.890 (90; 211), 2.781 (69; 221), 2.772 (67; 061), 2.601 (97; 023). It diffraction data on submicrometer sample. European Journal of was not possible to perform powder nor single-crystal X-ray diffraction Mineralogy, 31(2), 379–388.
    [Show full text]
  • List of Abbreviations
    List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote
    [Show full text]
  • Petrography and Engineering Properties of Igneous Rocks
    ENGINEERil~G MONOGRAPHS No. I United States Department of the Interior BUREAU OF RECLAMATION PETROGRAPIIY AND ENGINEERING· PROPER11ES OF IGNEOUS ROCKS hy Rit~bard C. 1\lielenz Denver, Colorado October 1948 95 cents (R.evised September 1961) United States Department of the Interior STEWART L. UDALL, Secretacy Bureau of Reclamation FLOYD E. DOMINY, Commissioner G~T BLOODGOOD, Assistant Commissioner and Chief Engineer Engineering Monograph No. 1 PETROGRAPHY AND ENGINEERING PROPERTIRES ·OF IGNEOUS RO<;:KS by Richard C. Mielenz Revised 1959. by William Y. Holland Head. Petrographic Laboratory Section Chemical Engineering Laboratory Branch Commissioner's Office. Denver Technical Infortnation Branch Denver Federal Center Denver, Colorado ENGINEERING MONOGRAPHS are published in limited editions for the technical staff of the Bureau of Reclamation and interested technical circles in Government and private agencies. Their purpose is to record devel­ opments, innovations, .and progress in the engineering and scientific techniques and practices that are employed in the planning, design, construction, and operation of Rec­ lamation structures and equipment. Copies 'may be obtained from the Bureau of Recla- · mation, Denver Federal Center, Denver, Colon.do, and Washington, D. C. Excavation and concreting of altered zones in rhyolite dike in the spillway foundation. Davis Damsite. Arizona-Nevada. Fl'ontispiece CONTENTS Page Introduction . 1 General Basis of Classification of Rocks . 1 Relation of the Petrographic Character to the Engineering Properties of Rocks . 3 Engineering J?roperties of Igneous Rocks ................................ :. 4 Plutonic Rocks . 4 Hypabyssal Rocks . 6 Volcanic Rocks..... 7 Application of Petrography to Engineering Problems of the Bureau of Reclamation . 8 A Mineralogic and Textural Classification of Igneous Rocks .
    [Show full text]
  • Mineral Index
    Mineral Index Abhurite T.73, T.355 Anandite-Zlvl, T.116, T.455 Actinolite T.115, T.475 Anandite-20r T.116, T.45S Adamite T.73,T.405, T.60S Ancylite-(Ce) T.74,T.35S Adelite T.115, T.40S Andalusite (VoU, T.52,T.22S), T.27S, T.60S Aegirine T.73, T.30S Andesine (VoU, T.58, T.22S), T.41S Aenigmatite T.115, T.46S Andorite T.74, T.31S Aerugite (VoU, T.64, T.22S), T.34S Andradite T.74, T.36S Agrellite T.115, T.47S Andremeyerite T.116, T.41S Aikinite T.73,T.27S, T.60S Andrewsite T.116, T.465 Akatoreite T.73, T.54S, T.615 Angelellite T.74,T.59S Akermanite T.73, T.33S Ankerite T.74,T.305 Aktashite T.73, T.36S Annite T.146, T.44S Albite T.73,T.30S, T.60S Anorthite T.74,T.415 Aleksite T.73, T.35S Anorthoclase T.74,T.30S, T.60S Alforsite T.73, T.325 Anthoinite T.74, T.31S Allactite T.73, T.38S Anthophyllite T.74, T.47S, T.61S Allanite-(Ce) T.146, T.51S Antigorite T.74,T.375, 60S Allanite-(La) T.115, T.44S Antlerite T.74, T.32S, T.60S Allanite-(Y) T.146, T.51S Apatite T.75, T.32S, T.60S Alleghanyite T.73, T.36S Aphthitalite T.75,T.42S, T.60 Allophane T.115, T.59S Apuanite T.75,T.34S Alluaudite T.115, T.45S Archerite T.75,T.31S Almandine T.73, T.36S Arctite T.146, T.53S Alstonite T.73,T.315 Arcubisite T.75, T.31S Althausite T.73,T.40S Ardaite T.75,T.39S Alumino-barroisite T.166, T.57S Ardennite T.166, T.55S Alumino-ferra-hornblende T.166, T.57S Arfvedsonite T.146, T.55S, T.61S Alumino-katophorite T.166, T.57S Argentojarosite T.116, T.45S Alumino-magnesio-hornblende T.159,T.555 Argentotennantite T.75,T.47S Alumino-taramite T.166, T.57S Argyrodite (VoU,
    [Show full text]
  • 39015003286252.Pdf
    raY a ... 3 4 _' J t+..,+1 /y s t O'C4 LOOM lescE NATUML- 010SIS OF THE TUNGSTEN EPOSITS OF THE UNITED STATES 4 Itoag tn February,. 1936 CONTENTS INTRODUCTION .. .. .............................. 1 LOCATION AND DISTRIBUTION ............................... 2 TYPES OF DEPOSITS OF COMMERCIAL TUNGSTEN ORE...........lO1 Pyrometasomatic deposits ................. ........ 10 Hypothermal deposits .................. S......0.12 Mesothermal deposits.......................... .12 Epithermal deposits...............................13 General features .... ............ .. .. .. 16 Non-Commercial Deposits .. .. ... .. ... ... .. .. .. ... .. 19 Segregation deposits .. .. ... .. .. ... .,.. .. .,.. .19 General features . ..... ....... .. .. .. 19 General features ......... ... .. .. .. .. .".". ."20 Associated minerals.. .. .". .. ."..".."""" 21 Commercial Deposits . .... * . .. .29.. Pyrometasomatic or contact-metamorphic deposits... .22 Location of deposits ............. "..... ... "". 23 Intrusive rocks. .. .23 CONTENTS (concluded) Sedimnrta~ry rocks. ... ......9" . 0 . .24 Process of contacte-metamorphism.0........ .... 24 Size and form of the deposits ................. 26 Zones of metamorphism.................. ".O".S" .26 Progression of the contact-metamorphism. ..... .27 General features and classification..g09.....28 Associated minerals............... "." " " ..... "29. Outcrop of tungsten veins.9......0.. 00"03 Downward extent of tungsten ve ins...........3 Gelaeenral.fatur.. .. .. ... .. .. ..... .. ........ 39 General features.......9. .
    [Show full text]