The Picking Table Volume 27, No. 1 – Spring 1986
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
TRAVERTINE-MARL DEPOSITS of the VALLEY and RIDGE PROVINCE of VIRGINIA - a PRELIMINARY REPORT David A
- Vol. 31 February 1985 No. 1 TRAVERTINE-MARL DEPOSITS OF THE VALLEY AND RIDGE PROVINCE OF VIRGINIA - A PRELIMINARY REPORT David A. Hubbard, Jr.1, William F. Gianninil and Michelle M. Lorah2 The travertine and marl deposits of Virginia's Valley and Ridge province are the result of precipitation of calcium carbonate from fresh water streams and springs. Travertine is white to light yellowish brown and has a massive or concretionary structure. Buildups of this material tend to form cascades or waterfalls along streams (Figure 1). Marl refers to white to dark yellowish brown, loose, earthy deposits of calcium carbonate (Figure 2). Deposits of these carbonate materials are related and have formed during the Quaternary period. This preliminary report is a compilation of some litei-ature and observations of these materials. A depositional model is proposed. These deposits have long been visited by man. Projectile points, pottery fragments, and firepits record the visitation of American Indians to Frederick and Augusta county sites. Thomas Jefferson (1825) wrote an account of the Falling Spring Falls from a visit prior to 1781. Aesthetic and economic considerations eontinue to attract interest in these deposits. 'Virginia Division of Mineral Resources, Charlot- Figure 1. Travertine waterfall and cascade series tesville, VA on Falling Springs Creek, Alleghany County, 2Department of Environmental Sciences, Univer- Virginia. Note man standing in center of left sity of Virginia, Charlottesville, VA margin. 2 VIRGINIA DIVISION OF MINERAL RESOURCES Vol. 31 Figure 2. An extensive marl deposit located in Figure 3. Rimstone dam form resulting from Frederick County, Virginia. Stream, in fore- precipitation of calcium carbonate in Mill Creek, ground, has incised and drained the deposit. -
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 -
Sussexite Mn2+BO2(OH)
2+ Sussexite Mn BO2(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As bladed acicular crystals, to 7 mm; cross-vein or radial fibrous, in felted or matted aggregates, nodular. Twinning: Submicroscopic twinning on {100} which cannot be resolved optically. Physical Properties: Tenacity: Inflexible. Hardness = 3–3.5 D(meas.) = 3.30 D(calc.) = 3.335 Optical Properties: Semitransparent. Color: White to buff, straw-yellow, pale pink; colorless in transmitted light. Streak: White. Luster: Silky, dull, earthy. Optical Class: Biaxial (–). Orientation: Parallel extinction; X = elongation; Z ⊥ flattening. Dispersion: r> v. α= 1.670 β = 1.728 γ = 1.732 2V(meas.) = ∼25◦ Cell Data: Space Group: P 21/a. a = 12.866(3) b = 10.718(2) c = 3.287(1) β =94.75(3)◦ Z=8 X-ray Powder Pattern: N’chwaning II mine, South Africa. 6.43 (10), 2.773 (7), 3.34 (6), 2.632 (6), 2.494 (6), 2.741 (5), 2.694 (5) Chemistry: (1) (3) B2O3 30.52 30.33 FeO 0.16 MnO 49.40 61.82 MgO 9.56 CaO 2.03 H2O 8.33 7.85 Total [100.00] 100.00 (1) Franklin, New Jersey, USA; recalculated to 100% after deduction of willemite 4.5%. (2) N’chwaning II mine, South Africa; by electron microprobe, analysis not given; stated to correspond to (Mn0.95Mg0.05)Σ=1.00BO2(OH). (3) MnBO2(OH). Polymorphism & Series: Forms a series with szaib´elyite. Occurrence: A rare hydrothermal mineral typically in veinlets in boron-bearing metamorphosed Mn–Fe–Zn deposits. -
MINERALS and MINERAL VARIETIES from METAMORPHOSED Mn DEPOSITS of BISTRITA MOUNTAINS, ROMANIA
Acta Mineralogica-Petrographica, Abstract Series 1, Szeged, 2003 MINERALS AND MINERAL VARIETIES FROM METAMORPHOSED Mn DEPOSITS OF BISTRITA MOUNTAINS, ROMANIA HÎRTOPANU, P.1 & SCOTT, P.2 1 Geological Institute of Romania, Caransebeş 1, RO-78344 Bucharest, Romania. E-mail: [email protected] 2 Camborne School of Mines, Redruth, Cornwall, United Kingdom. The Bistrita Mountains belong to the Crystalline Meso- mation of some amphiboles and some pyroxenes into other zoic Zone of the East Carpathians, which consists of super- phases, there are drastical transformations of pyroxenes into posed Variscan and Alpine Nappes, overthrusted eastwards pyroxenoids (johannsenite into rhodonite), pyroxenoids into over the Flysch Zone. The manganese ore is contained by pyroxenoids (pyroxmangite into rhodonite), pyroxmangite Tulghes Group (Tg2 level) of the Variscan Putna Nappe, into manganogrunerite, garnets into garnets (spessartine- situated over the Pietrosu Bistritei Nappe and supporting the calderite into spessartine, spessartine into anisotropic spes- thrusting of the Rebra Nappe. All these Variscan nappes sartine-andradite-grossular), calderite into pyroxmangite- constitute the Alpine Sub-Bucovinian Nappe localised be- magnetite, etc. are the best evidences of continuous variation tween Alpine Infrabucovinian Nappe in the East and the of formation conditions. Alpine Bucovinian Nappe in the West. The Mn ore have a predominant carbonate rather than The mineralogy of Mn metamorphosed deposits from silicate mineralogical composition, which means a great CO2 Bistrita Mts. includes 328 minerals and mineral varieties. fluid control in the carbonation and dehydration processes They may count among the mineralogically the most com- along the many stages of the whole history of the ore and the plex deposits of the world. -
Kinoshitalite (Ba,K)(Mg,Mn,Al)3Si2al2o10(OH)2
Kinoshitalite (Ba; K)(Mg; Mn; Al)3Si2Al2O10(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Forms small scales, < 1 mm. Physical Properties: Cleavage: 001 , perfect. Tenacity: Brittle. Hardness = 2.5{3 D(meas.) = 3.30 D(calc.) = 3.33 f g Optical Properties: Semitransparent. Color: Yellow-brown to colorless; light yellow to colorless in thin section. Luster: Vitreous. Optical Class: Biaxial ({). Pleochroism: X = very light yellow to light yellow; Y = Z = light yellow with brownish tinge. Absorption: Y Z > X. ® = 1.619 ¯ = 1.628{1.633 ° = 1.635 ' 2V(meas.) = 23± Cell Data: Space Group: C2=m: a = 5.345(3) b = 9.250(4) c = 10.256(8) ¯ = 99:99(6)± Z = 2 X-ray Powder Pattern: Noda-Tamagawa mine, Japan. 3.37 (100), 2.52 (55), 2.020 (55), 5.05 (50), 10.1 (45), 1.684 (15), 3.16 (5) Chemistry: (1) (2) (1) (2) SiO2 24.58 23.43 BaO 17.85 27.60 TiO2 0.16 Na2O 0.68 0.11 Al2O3 22.06 19.25 K2O 3.30 0.24 Fe2O3 0.71 1.87 F 0.21 + Mn2O3 3.24 H2O 2.90 FeO 0.04 H2O¡ 0.20 MnO 7.38 2.62 H2O 3.50 MgO 16.60 21.95 O = F 0.09 ¡ 2 CaO 0.05 0.05 Total 99.87 100.62 2+ (1) Noda-Tamagawa mine, Japan; corresponds to (Ba0:58K0:35Na0:11Ca0:01)§=1:05(Mg2:06Mn0:52 3+ 3+ Al0:22Mn0:21Fe0:04Ti0:01)§=3:06Si2:05Al1:94O10[(OH)1:62O0:33F0:06]§=2:01: (2) Netra, India; by electron microprobe, total Fe as Fe2O3; corresponding to (Ba0:93K0:03Na0:02Ca0:01)§=0:99 (Mg2:80Mn0:19Fe0:08)§=3:07Si2:01(Al1:94Fe0:05)§=1:99O10(OH)2: Polymorphism & Series: 1M, 2M1 polytypes. -
Download the Scanned
American Mineralogist, Volume 70, pages 379-387, 1985 Ma_nganesehumites and leucophoenicitesfrom Franklin and Sterling- Hill' NewJersev: 'i"? andimplications ;ifi':il1,;;lfiil11"r's' Perr J. Dullx Department of Mineral Sciences Smithsonian lnstitution, Washington, D. C. 20560 Abstract The manganesehumites, (alleghanyite, manganhumite, and sonolite),together with some Mn-bearing samplesof the Mg-humites,and the related phasesleucophoenicite and jerry- gibbsite,from the orebodiesat Franklin and SterlingHill, New Jersey,are describedtogether with analytical data. Solid solution betweenhumite and manganhumiteis at least partially continuous. Expected Mn/Mg solid solutions between alleghanyiteand chondrodite, and betweensonolite and clinohumite, are discontinuous; they are interrupted by apparently orderedphases. In all cases,the possibleorderings involve Zn as well as Mn and Mg. There are no Mn end-membersof the manganesehumites at this locality. Manganeseis apparently restricted in leucophoenicite(5.42-6.63 Mn per 7 octahedral cations) and in jerrygibbsite (7.79-8.02Mn per 9 octahedralcations). Calcium is common to both leucophoeniciteand jerrygibbsite,but among the Mn-humites,only sonoliteaccepts appreciable Ca (0.65Ca per 9 octahedralcations). There is a "threshold" level ofzinc in all studiedsamples; this "threshold" levelis a constantfor leucophoenicite1-9.3 Znper 3 Si)and alleghanyite(-O.2Zn per 2 Si). No samplesof leucophoeniciteor jerrygibbsite were found to be Zn-ftee,suggesting either that Zn is required for their stability, or that these two phasesmight not be stable as end-members.Fluorine is present in all the Mn-humites and is proportional to the Mg- content,but is absentin leucophoeniciteand jerrygibbsite. Introduction humite speciesoccur there; the Mg-humites occur in the The magnesiumhumite species(norbergite, chondrodite, host Franklin Marble for the most part, and the Mn- humite, and clinohumite) have been well-studiedand re- humites in the orebodiesthemselves. -
Kumtyubeite Ca5(Sio4)2F2—A New Calcium Mineral of the Humite Group from Northern Caucasus, Kabardino-Balkaria, Russia
American Mineralogist, Volume 94, pages 1361–1370, 2009 Kumtyubeite Ca5(SiO4)2F2—A new calcium mineral of the humite group from Northern Caucasus, Kabardino-Balkaria, Russia Ir I n a О. Ga l u s k I n a ,1,* BI l j a n a la z I c ,2 Th o m a s ar m B r u s T e r,2 ev G e n y v. Ga l u s k I n ,1 vI k T o r m. Ga z e e v,3 al e k s a n d e r e. za d o v,4 nI k o l a I n. Pe r T s e v,3 lIdIa je ż a k ,5 ro m a n Wr z a l I k ,6 a n d an a T o l y G. Gu r B a n o v 3 1Faculty of Earth Sciences, Department of Geochemistry, Mineralogy and Petrography, University of Silesia, Będzińska 60, 41-200 Sosnowiec, Poland 2Mineralogical Crystallography, Institute of Geological Sciences, University of Bern, Freiestrasse 3, CH-3012 Bern, Switzerland 3Institute of Geology of Ore Deposits, Geochemistry, Mineralogy and Petrography (IGEM) RAS, Staromonetny 35, 119017 Moscow, Russia 4OOO NPP TEPLOCHIM, Dmitrovskoye av. 71, 127238 Moscow, Russia 5Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw, al. Żwirki i Wigury 93, 02-089 Warszawa, Poland 6Institute of Physics, University of Silesia, Uniwersytecka 4, 40-007 Katowice, Poland aB s T r a c T Kumtyubeite, Ca5(SiO4)2F2—the fluorine analog of reinhardbraunsite with a chondrodite-type structure—is a rock-forming mineral found in skarn carbonate-xenoliths in ignimbrites of the Upper Chegem volcanic structure, Kabardino-Balkaria, Northern Caucasus, Russia. -
Leucophoenicite Mn (Sio4)3(OH)2
2+ Leucophoenicite Mn7 (SiO4)3(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Crystals rare, typically slender, prismatic, elongated and striated [010], to 8 mm; in isolated grains or granular massive. Twinning: On k 001 , common, contact or interpenetrant twins, lamellar. f g Physical Properties: Cleavage: 001 , imperfect. Tenacity: Brittle. Hardness = 5.5{6 f g D(meas.) = 3.848 D(calc.) = [4.01] Optical Properties: Transparent to translucent. Color: Brown to light purple-red, raspberry-red, deep pink to light pink; rose-red to colorless in thin section. Luster: Vitreous. Optical Class: Biaxial ({). Pleochroism: Faint; rose-red 001 ; colorless 001 . Orientation: k f g ? f g X 001 cleavage. Dispersion: r > v; slight. ® = 1.751(3) ¯ = 1.771(3) ° = 1.782(3) ? f g 2V(meas.) = 74(5)± Cell Data: Space Group: P 21=a: a = 10.842(19) b = 4.826(6) c = 11.324(9) ¯ = 103:93(9)± Z = [2] X-ray Powder Pattern: Franklin, New Jersey, USA. 1.8063 (10), 2.877 (9), 2.684 (8), 4.36 (5), 3.612 (5), 2.365 (5), 2.620 (4) Chemistry: (1) (2) (3) (1) (2) (3) SiO2 26.36 26.7 26.7 CaO 5.67 2.4 2.8 FeO trace 0.3 0.3 Na2O 0.39 MnO 60.63 62.8 64.7 K2O 0.24 ZnO 3.87 0.0 0.0 H2O 2.64 [2.3] [2.8] MgO 0.21 5.5 2.7 Total 100.01 [100.0] [100.0] (1) Franklin, New Jersey, USA; composite of two analyses, corresponding to (Mn5:89Ca0:70Zn0:32 Na0:04Mg0:03K0:01)§=6:99(Si1:01O4)3(OH)2: (2) Kombat mine, Namibia; by electron microprobe, H2O by di®erence; corresponding to (Mn5:98Mg0:92Ca0:29Fe0:02)§=7:21(SiO4)3(OH)1:72: (3) Valsesia-Valtournanche area, Italy; by electron microprobe, H2O by di®erence; corresponding to (Mn6:16Mg0:45Ca0:34Fe0:03)§=6:98(SiO4)3(OH)2:10: Mineral Group: Leucophoenicite group. -
The Picking Table Volume 8, No. 1
THE PICKING TABLE FRANKLIN OGDENSBURG MINSHALOGICAL SOCIETY, INC, P. 0. BOJC 146 FRANKLIN, H.J., 07416 VOLUME VIII FEBRUARY 196? NUMBER 1 The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. CLUB PROGRAM - SPRING 1967 All meetings will be held at the Hardyston School, intersection of Routes #23 and #517, Franklin, N. J. Pre meeting activities start at 1:00 P.A. Speaker will be announced at 2:30 P.M. Sunday, Field trip, 9=00 A..-I. to Noon - March 19th. Buckwheat Dump, Franklin, N.J. Meeting, 2:30 P.M. Speaker, Paul Desautels Subject - Blood Relatives Among the Minerals. Saturday, Field trip, 9:00 A.M. to Noon - April 15th Buckwheat Dump, Franklin, N.J. Meeting, 2:30 P.M. Speaker - Dr. Paul Moore. Subject - The Mineralogy of Langban, Sweden. Saturday, Field trip, 9:00 A.M. to Noon - Open Cuts, May 20th Sterling Hill Mine, Ogdensburg, H. J. Meeting, 2:30 P.M. Speaker - Dr. Clifford Frondel Subject - Franklin Minerals, New and Old Saturday, Field trio, 9:00 A.M. to Noon - June 17th Farber Quarry, Cork Hill Road, Franklin, ..J, Meeting, 2:30 P.JL Speaker - Robert Metsger Subject - The Geology of Sterling Hill. Special Events April 22/23 1967 Earth Science and Gem Show Mineralogical Society of Pennsylvania, Route 30, Lancaster, Pa. May 6/7th 3rd Annual Mineral and Gem Show Matawan Mineralogical Society, Matawan Regional High School, Matawan, ft. June 29/July 2nd 1967 National Gem and Mineral Show, Eastern Federation, Washington Hilton Hotel, Washington, D.C. -
H Positions in Leucophoenicite, Mn7si3o12(OH)2: a Close Relative of the Hydrous B Phases
American Mineralogist, Volume 87, pages 154–159, 2002 H positions in leucophoenicite, Mn7Si3O12(OH)2: A close relative of the hydrous B phases MARK D. WELCH,1,* WILLIAM G. MARSHALL,2 NANCY L. ROSS,3 AND KEVIN S. KNIGHT2 1Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, U.K. 2ISIS Facility, Rutherford Appleton Laboratory, Chilton, Didcot, Oxon OX11 0QX, U.K. 3Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061, U.S.A. ABSTRACT The proton positions in leucophoenicite, ideally Mn7Si3O12(OH)2, have been determined by neu- tron powder diffraction under ambient conditions on a natural sample from Franklin, New Jersey. 2 Refinement in the P21/a space group gave Rp = 2.0% (wRp = 2.1%), χ = 4.04 for 110 refined param- eters. The two non-equivalent protons form a pair of hydroxyl groups and make hydrogen bonds to the same O7 atom of the Si1 tetrahedron at distances of 1.99(1) and 2.09(1) Å. The H····H distance in leucophoenicite is 2.16(1) Å, which is more than twice the Van der Waal’s radius of H (>2 Å) and so no proton positional disorder is expected in leucophoenicite. A comparison of the H environments is made between leucophoenicite and Phase B, Superhydrous B, and Phase A. INTRODUCTION tions of cation octahedra in leucophoenicite are like those of Understanding the behavior of hydrogenous components of the hydrous sheet of Phase B. The leucophoenicite structure mantle phases is important for interpreting the crystal chemis- consists of two polyhedral sheets which, in the centrosymmet- try and physical properties (elasticity and rheology) of these ric structure (see below), are related by inversion centers. -
Jerrygibbsite Mn (Sio4)
2+ Jerrygibbsite Mn9 (SiO4)4(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Orthorhombic. Point Group: mm2 (probable), or 2=m 2=m 2=m: As interlocking anhedral crystals, to 2 mm. Physical Properties: Cleavage: Imperfect on 001 . Hardness = 5.5 D(meas.) = 4.00(2) D(calc.) = 4.045 f g » Optical Properties: Transparent and translucent lamellae alternating 001 . Color: Violet-pink, with a brownish tinge; light pink in thin section. Strekakf: Light pink. Luster: Vitreous. Optical Class: Biaxial ({). Orientation: X = b; Y = c; Z = a. Dispersion: r > v; moderate. ® = 1.772(4) ¯ = 1.783(4) ° = 1.789(4) 2V(meas.) = 72± Cell Data: Space Group: P bn21 (probable), or P bnm: a = 4.875(2) b = 10.709(6) c = 28.18(2) Z = 4 X-ray Powder Pattern: Franklin, New Jersey, USA. 2.557 (100), 1.806 (100), 2.869 (78), 2.752 (49), 2.702 (46), 2.362 (39), 2.661 (34) Chemistry: (1) SiO2 27.1 FeO 0.3 MnO 64.1 ZnO 3.9 MgO 1.4 CaO 0.4 F 0.0 H2O 2.13 Total 99.3 (1) Franklin, New Jersey, USA; by electron microprobe, H2O by the Pen¯eld method; corresponds to (Mn7:86Zn0:59Mg0:24Ca0:16Fe0:14)§=8:99(SiO4)4(OH)2: Polymorphism & Series: Dimorphous with sonolite. Mineral Group: Leucophoenicite group. Occurrence: In a metamorphosed stratiform Zn-Mn deposit. Association: Franklinite, willemite, zincite, sonolite, leucophoenicite, tephroite. Distribution: From Franklin, Sussex Co., New Jersey, USA. Name: In honor of Professor Gerald V. Gibbs, Virginia Polytechnic Institute and State University, Blacksburg, Virginia, USA. -
A Mineral Resembling Meerschaum from the Serpentine Range of Hampden County, Mass., with the Descriptions of Interesting Included Crystals
Journal of the Minnesota Academy of Science Volume 4 Number 2 Article 2 1899 A Mineral Resembling Meerschaum From the Serpentine Range of Hampden County, Mass., With the Descriptions of Interesting Included Crystals. A. D. Roe Follow this and additional works at: https://digitalcommons.morris.umn.edu/jmas Part of the Earth Sciences Commons Recommended Citation Roe, A. D. (1899). A Mineral Resembling Meerschaum From the Serpentine Range of Hampden County, Mass., With the Descriptions of Interesting Included Crystals.. Journal of the Minnesota Academy of Science, Vol. 4 No.2, 268-276. Retrieved from https://digitalcommons.morris.umn.edu/jmas/vol4/iss2/2 This Article is brought to you for free and open access by the Journals at University of Minnesota Morris Digital Well. It has been accepted for inclusion in Journal of the Minnesota Academy of Science by an authorized editor of University of Minnesota Morris Digital Well. For more information, please contact [email protected]. • Mineral Resembling Meerschaum and Baffin 's Land, so that the same shore line had run through these three places. Pro fessor Arndt reported o n his investigations into orig inal m ethods of tcarhing science. H . Gale reported on the interesting picture of scientific activity. mingled with a broad culture, found in the delightful •· Briefe von Dr. T h co. Billroth.'' 276th Meeting, November, 1905. Secretary 's minut es lacking. Paper L , P sy chology of the Busines s Man hv•• Harlow Gale. 277th Meeting, December s, 1905. Secretary 's minutes lacking . Paper M. Glacial and l\Iorlified D rift of the ~[i ss i :;sipp i Valley from Lake Itasca to Lake Pepin, by \•\ 'arren Upham .