The Importance of Proper Crystal-Chemical and Geometrical Reasoning Demonstrated Using Layered Single and Double Hydroxides
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Minerals of the Hydrotalcite Group in Metasomatically Altered Carbonate Rocks from Zawiercie, S Poland
MINERALOGIA POLONICA Vol. 32, No 1, 2001 PL ISSSN 0032-6267 Ewa KOSZOWSKA1, Dorota SAŁATA1 MINERALS OF THE HYDROTALCITE GROUP IN METASOMATICALLY ALTERED CARBONATE ROCKS FROM ZAWIERCIE, S POLAND A b s t a c t . Minerals of the hydrotalcite-manasseite group were identified in samples from two borehols in Zawiercie (ZMZ-9, RK-1). The minerals were found in calciphire bodies (RK-1) and in one small, metasomatic veinlet (ZMZ-9) formed in Middle Devonian dolomites. Alteration of dolomitic sediments was genetically connected with infiltration fluids that caused formation of a gamet-pyroxene skam. Inves tigations have revealed the presence of both hydrotalcite and manasseite. Besides, in few places of the veinlet there occurs a mineral, which has been recognized as iowaite. Key-words: hydrotalcite-manasseite group, calciphires, ska ms, metasomatic veins, Zawiercie, S Poland INTRODUCTION The hydrotalcite group minerals belong to a large group of natural and synthetic dihydroxides named also as "layered double hydroxides" or "anionic clays". Their general formula can be written as: M |2XM (0 H)2 (Am“)x/mn H 2 0 (where M+2, M +3 are cations in the hydroxide layers and Am_ is the interlayer anion) and is based on positively charged brucite-like layers with C 03-like anions and water molecules in interlayer positions (Drits et al. 1987) (Fig. la). Within the group, depending on the composition of the octahedral brucite-type cationic layers, three subgroups can be distinguished in which the cations are: a) M g +2 + Al+3, b) Mg +2 + Fe+3 , c) M g + 2 + C r+3. -
Genesis of the Brecciated Rocks from Mid Atlantic Ridge Hydrothermal Systems: Lucky Strike (37º20’N) and Menez Gwen (37º50’N)
UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS DEPARTAMENTO DE GEOLOGIA GENESIS OF THE BRECCIATED ROCKS FROM MID ATLANTIC RIDGE HYDROTHERMAL SYSTEMS: LUCKY STRIKE (37º20’N) AND MENEZ GWEN (37º50’N) Isabel Maria Amaral Costa Doutoramento em Geologia na especialidade de Metalogenia 2013 UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS DEPARTAMENTO DE GEOLOGIA GENESIS OF THE BRECCIATED ROCKS FROM MID ATLANTIC RIDGE HYDROTHERMAL SYSTEMS: LUCKY STRIKE (37º20’N) AND MENEZ GWEN (37º50’N) Isabel Maria Amaral Costa Tese orientada pelo Prof. Doutor Fernando José Arraiano de Sousa Barriga especialmente elaborada para a obtenção do grau de Doutor em Geologia na especialidade de Metalogenia 2013 To my parents and grandmother After climbing a great hill, one only finds that there are many more hills to climb. Nelson Mandela, sometime, somewhere in South Africa Acknowledgements The work presented here was only possible due to the collaboration of different people and institutions. My first acknowledgement goes to Professor Fernando Barriga, my Ph. D supervisor. His guidance and support during the long period of this work were important to overcome the several difficulties that arose. His belief in the successful completion of this thesis and the logistic support were essential. I also acknowledge the support of Doctor Yves Fouquet in giving me the chance to develop some of the thesis studies in “Institut Français de Recherche pour l'Exploitation de la MER” (IFREMER) and for his scientific guidance. To “Fundação para a Ciência e a Tecnologia” (FCT) I am grateful for the financial support through a PhD scholarship (PRAXIS/BD/9408/96). I am also indebted to the financial support of CREMINER LARSyS and to the logistic support of “Faculdade de Ciências da Universidade de Lisboa” (FCUL). -
Infrare D Transmission Spectra of Carbonate Minerals
Infrare d Transmission Spectra of Carbonate Mineral s THE NATURAL HISTORY MUSEUM Infrare d Transmission Spectra of Carbonate Mineral s G. C. Jones Department of Mineralogy The Natural History Museum London, UK and B. Jackson Department of Geology Royal Museum of Scotland Edinburgh, UK A collaborative project of The Natural History Museum and National Museums of Scotland E3 SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. Firs t editio n 1 993 © 1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 1st edition 1993 Typese t at the Natura l Histor y Museu m ISBN 978-94-010-4940-5 ISBN 978-94-011-2120-0 (eBook) DOI 10.1007/978-94-011-2120-0 Apar t fro m any fair dealin g for the purpose s of researc h or privat e study , or criticis m or review , as permitte d unde r the UK Copyrigh t Design s and Patent s Act , 1988, thi s publicatio n may not be reproduced , stored , or transmitted , in any for m or by any means , withou t the prio r permissio n in writin g of the publishers , or in the case of reprographi c reproductio n onl y in accordanc e wit h the term s of the licence s issue d by the Copyrigh t Licensin g Agenc y in the UK, or in accordanc e wit h the term s of licence s issue d by the appropriat e Reproductio n Right s Organizatio n outsid e the UK. Enquirie s concernin g reproductio n outsid e the term s state d here shoul d be sent to the publisher s at the Londo n addres s printe d on thi s page. -
New Mineral Names*
American Mineralogist, Volume 97, pages 2064–2072, 2012 New Mineral Names* G. DIEGO GATTA,1 FERNANDO CÁMARA,2 KIMBERLY T. TAIT,3,† AND DMITRY BELAKOVSKIY4 1Dipartimento Scienze della Terra, Università degli Studi di Milano, Via Botticelli, 23-20133 Milano, Italy 2Dipartimento di Scienze della Terra, Università di degli Studi di Torino, Via Valperga Caluso, 35-10125 Torino, Italy 3Department of Natual History, Royal Ontario Museum, 100 Queens Park, Toronto, Ontario M5S 2C6, Canada 4Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia IN THIS ISSUE This New Mineral Names has entries for 12 new minerals, including: agardite-(Nd), ammineite, byzantievite, chibaite, ferroericssonite, fluor-dravite, fluorocronite, litochlebite, magnesioneptunite, manitobaite, orlovite, and tashelgite. These new minerals come from several different journals: Canadian Mineralogist, European Journal of Mineralogy, Journal of Geosciences, Mineralogical Magazine, Nature Communications, Novye dannye o mineralakh (New data on minerals), and Zap. Ross. Mineral. Obshch. We also include seven entries of new data. AGARDITE-(ND)* clusters up to 2 mm across. Agardite-(Nd) is transparent, light I.V. Pekov, N.V. Chukanov, A.E. Zadov, P. Voudouris, A. bluish green (turquoise-colored) in aggregates to almost color- Magganas, and A. Katerinopoulos (2011) Agardite-(Nd), less in separate thin needles or fibers. Streak is white. Luster is vitreous in relatively thick crystals and silky in aggregates. Mohs NdCu6(AsO4)3(OH)6·3H2O, from the Hilarion Mine, Lavrion, Greece: mineral description and chemical relations with other hardness is <3. Crystals are brittle, cleavage nor parting were members of the agardite–zálesíite solid-solution system. observed, fracture is uneven. Density could not be measured Journal of Geosciences, 57, 249–255. -
Motukoreaite Na2mg38al24(SO4)8(CO3)13(OH)108 • 56H2O C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Hexagonal
Motukoreaite Na2Mg38Al24(SO4)8(CO3)13(OH)108 • 56H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 32/m. As tabular hexagonal crystals, showing rounded {0001} and possible {1120}, {1011}, {1014}, to 0.2 mm, forming rosettes, boxworks, and subparallel aggregates, and as a claylike cement. Physical Properties: Cleavage: Good on {0001}, perhaps a parting. Tenacity: Sectile, flexible. Hardness = 1–1.5 D(meas.) = 1.43–1.53 D(calc.) = 1.478 Partial dehydration readily occurs. Optical Properties: Semitransparent. Color: Colorless, white, pale yellow, pale yellow-green. Luster: Dull. Optical Class: Uniaxial (+), nearly isotropic. n = ∼1.51, birefringence ∼0.012. ω = n.d. = n.d. Cell Data: Space Group: R3m. a = 9.172(2) c = 33.51(1) Z = 3 X-ray Powder Pattern: Brown’s Island, New Zealand; may exhibit preferred orientation. 11.32 (vvs), 5.58 (s), 4.59 (s), 3.72 (s), 2.578 (s), 2.386 (s), 2.158 (s) Chemistry: (1) (2) (1) (2) SO3 10.00 10.65 CaO 0.92 SiO2 5.55 Na2O 0.71 1.03 CO2 9.32 9.52 K2O 0.10 + Al2O3 17.87 20.35 H2O 19.62 − Fe2O3 0.73 H2O 10.35 MnO 0.70 H2O 32.97 ZnO 0.56 Total 99.41 100.00 MgO 22.98 25.48 (1) Brown’s Island, New Zealand; contains estimated quartz 5%, traces of calcite and goethite; after removal of probable impurities, and with (OH)1− calculated for charge balance, corresponds • to (Na1.50K0.14)Σ=1.64Mg37.36Al22.97(SO4)8.18(CO3)13.81(OH)101.29 58.36H2O. -
THE CRYSTAL STRUCTURE of SHIGAITE, Lalmne*(Oh)Ele(So+Lzna(H2o)6{H2o}6, a HYDROTALCITE.GROUP MINERAL
9L The CanadianMineralo gist Vol. 34, pp. 91,-97(1996) THE CRYSTALSTRUCTURE OF SHIGAITE, lAlMne*(oH)ele(so+lzNa(H2o)6{H2o}6, A HYDROTALCITE.GROUPMINERAL MARK A. COOPERand FRANK C. HAWTHORNE Deparnnewof GeolagicalSciences, University of Manitoba"Winnipeg, Manitoba, R3T 2N2 ABSTRACT The cryslal strucbre of shigaite, tAMnA+(OlD6l3(SOfrNa(H2O)6{HzO}0,rhombohedral, a 9.512(l), c 33.074$) 4,, y 2591.0(8) Ar, Z = 3, R3, hasbeen solved by direct nethods and refined to an R ndex of 4.2Vousing 979 observedreflections measuredwith MoKcl X-radiation.The structuralunit of shigaiteis a planar sheetof edge-sharingoctahedra [AlMna+(OID6]1+. These oxycation sheetsare intercalatedwith oxyanion she€tsof chemical composition Na(H2O)6{H2O}6(SOf2;hydrogen bonding plays a major role in linkage both within the oxyanionsheet and betweenthe structuraluoit and the oxyanionsheet of interstitial species.This work showsshigaite to containessential Na andresults in a significantrevision ofthe chemicalformula- Shigaiteis a hydrotalcite-goup mineral, the Mn2+analogue of motukoreaite. Keywords:shigaite, crystal structure,chemical formul4 hydrogenbonding, hydrotalcite group. Somaanr Nous avons affin6 la stucture de la shigarte, IA1MnS+(OII)613(SO)2Na(H2O)6{HzO}0,rhombo6drique, a 9.512(l), c 33.074(0A, V259L.09)N,z= 3, Rl parm6thoaes directeijusqu'lirnreiiiu n a6l.Z%6nuinsnt979 r6flexionsobserv6es avecun rayonnementMorcr. L'unit6 structuraleest un feuillet d'octabdrese a€tes partag6es,de composition[AlMn3+(OI{)6]11 Ces couchesoxy-cationiques sont intercal6esavec des couchesoxy-anioniques de composition Na(H2O)6{H2O}6(SO)2; les liaisons hydrogdnejouent un role imporanq aussi bien dsns les couchesoxy-anioniques qu'enhe I'unit6 structuraleet la coucheoxy-anionique de I'espbceinterstitielle. -
Chemistry, Geochemistry, and Geology of Chromium and Chromium Compounds
L1608_C02.fm Page 23 Thursday, July 15, 2004 6:57 PM 2 Chemistry, Geochemistry, and Geology of Chromium and Chromium Compounds William E. Motzer and Todd Engineers CONTENTS 2.1 Chromium Chemistry .................................................................................24 2.1.1 Background ......................................................................................24 2.1.2 Elemental/Metallic Chromium Characteristics .........................25 2.1.3 Ionic Radii ........................................................................................29 2.1.4 Oxidation States...............................................................................30 2.1.5 Stable and Radioactive Isotopes ...................................................31 2.1.6 Characteristics of Chromium Compounds.................................34 2.2 Natural Chromium Concentrations..........................................................34 2.2.1 Mantle ...............................................................................................46 2.2.2 Chromium Minerals........................................................................46 2.2.3 Chromium Ore Deposits................................................................46 2.2.3.1 Stratiform Mafic-Ultramafic Chromite Deposits .........62 2.2.3.2 Podiform- or Alpine-Type Chromite Deposits ............63 2.2.4 Crude Oil, Tars and Pitch, Asphalts, and Coal..........................63 2.2.5 Rock ...................................................................................................64 -
C:\Documents and Settings\Alan Smithee\My Documents\MOTM
Itkx1//7Lhmdq`knesgdLnmsg9Rshbgshsd Our ongoing search for new minerals to feature finds us scouring the more than forty separate shows that comprise the Tucson Gem & Mineral show every year, looking for large lots of interesting and attractive minerals. The search is rewarded when we make a new contact and find something especially vibrant like this month’s combination of lavender stichtite in green serpentinite! OGXRHB@K OQNODQSHDR Chemistry: Mg6Cr2(CO3)(OH)16A4H2O Basic Hydrous Magnesium Chromium Carbonate (Hydrous Magnesium Chromium Carbonate Hydroxide) Class: Carbonates Subclass: Carbonates with hydroxyl or halogen radicals Group: Hydrotalcite Crystal System: Trigonal Crystal Habits: Crystals rarely macroscopic; usually as crust-like aggregates in matrix; sometimes radiating, micaceous with flexible plates, and nodular with tuberous, irregular surface projections; also massive and fibrous. Color: Lavender, lilac, light violet, pink, or purplish. Luster: Waxy, greasy, sometimes pearly. Transparency: Transparent to translucent Streak: White to pale lilac Refractive Index: 1.516-1.542 Cleavage: Perfect in one direction Fracture: Uneven, brittle. Hardness: 1.5-2.0 Specific Gravity: 2.2 Luminescence: None Distinctive Features and Tests: Softness, color, crystal habits, occurrence in chromium-rich metamorphic environments, and frequent association with serpentinite (a greenish metamorphic rock). Stichtite can be confused with similarly colored sugilite [potassium sodium iron manganese aluminum lithium silicate, KNa2(Fe,Mn,Al)2Li2Si12O30]. -
Stichtite Mg6cr2co3(OH)16∙4H2O - Crystal Data: Hexagonal
Stichtite Mg6Cr2CO3(OH)16∙4H2O - Crystal Data: Hexagonal. Point Group: 3 2/m or 6/m 2/m 2/m. As aggregates of fibers or plates, commonly matted, contorted; as cross-fiber veinlets and micaceous scales. Physical Properties: Cleavage: Perfect on {0001}. Tenacity: Laminae flexible, not elastic; greasy feel. Hardness = 1.5-2 D(meas.) = 2.16 D(calc.) = 2.11 Optical Properties: Transparent. Color: Lilac to rose-pink; lilac to rose-pink in transmitted light. Streak: Very pale lilac to white. Luster: Waxy to resinous, somewhat pearly. Optical Class: Uniaxial (–); may be anomalously biaxial. ω = 1.545(3) ε = 1.518(3) 2V(meas.) = Small. Pleochroism: Weak; O = dark rose-pink to lilac; E = light rose-pink to lilac. - Cell Data: Space Group: R3 m. a = 3.09575(3) c = 23.5069(6) Z = 3/8 (stichtite-3R) Space Group: P63/mmc. a = 3.09689(6) c = 15.6193(8) Z = 1/4 (stichtite-2H) X-ray Powder Pattern: Dundas, Tasmania, Australia. (ICDD 14-330) 7.8 (100), 3.91 (90), 2.60 (40), 2.32 (30), 1.97 (30), 1.54 (20), 1.51 (20) Chemistry: (1) (2) Al2O3 2.30 Fe2O3 4.18 Cr2O3 14.15 23.24 MgO 37.72 36.98 H2O 34.14 33.05 CO2 7.15 6.73 Total [100.00] 100.00 (1) Dundas, Tasmania, Australia; probably intermixed with stichtite-2H, original total of 99.27% recalculated to 100% after deduction of SiO2 2.09%, FeO 0.28% as chromite. (2) Mg6Cr2(CO3)(OH)16•4H2O. Polymorphism & Series: Polytypes 3R and 2H (formerly barbertonite). -
A Specific Gravity Index for Minerats
A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951). -
12Cl23h2o, a New Gibbsite-Based Hydrotalcite Supergroup
minerals Article Dritsite, Li2Al4(OH)12Cl2·3H2O, a New Gibbsite-Based Hydrotalcite Supergroup Mineral Elena S. Zhitova 1,2,* , Igor V. Pekov 3, Ilya I. Chaikovskiy 4, Elena P. Chirkova 4, Vasiliy O. Yapaskurt 3, Yana V. Bychkova 3, Dmitry I. Belakovskiy 5, Nikita V. Chukanov 6, Natalia V. Zubkova 3, Sergey V. Krivovichev 1,7 and Vladimir N. Bocharov 8 1 Department of Crystallography, St. Petersburg State University, Universitetskaya nab. 7/9, St. Petersburg 199034, Russia 2 Laboratory of Mineralogy, Institute of Volcanology and Seismology, Russian Academy of Sciences, Bulvar Piypa 9, Petropavlovsk-Kamchatsky 683006, Russia 3 Faculty of Geology, Moscow State University, Vorobievy Gory, Moscow 119991, Russia 4 Mining Institute, Ural Branch of the Russian Academy of Sciences, Sibirskaya str., 78a, Perm 614007, Russia 5 Fersman Mineralogical Museum, Russian Academy of Sciences, Leninsky Prospekt 18-2, Moscow 119071, Russia 6 Institute of Problems of Chemical Physics, Russian Academy of Sciences, Akad. Semenova 1, Chernogolovka, Moscow Region 142432, Russia 7 Nanomaterials Research Centre, Kola Science Centre, Russian Academy of Sciences, Fersman Street 14, Apatity 184209, Russia 8 Resource Center Geomodel, St. Petersburg State University, Universitetskaya nab. 7/9, St. Petersburg 199034, Russia * Correspondence: [email protected]; Tel.: +7-924-587-51-91 Received: 2 August 2019; Accepted: 14 August 2019; Published: 17 August 2019 Abstract: Dritsite, ideally Li Al (OH) Cl 3H O, is a new hydrotalcite supergroup mineral formed 2 4 12 2· 2 as a result of diagenesis in the halite carnallite rock of the Verkhnekamskoe salt deposit, Perm Krai, − Russia. Dritsite forms single lamellar or tabular hexagonal crystals up to 0.25 mm across. -
Systematics and Crystal Genesis of Carbonate Minerals
ГОДИШНИК НА МИННО-ГЕОЛОЖКИЯ УНИВЕРСИТЕТ “СВ. ИВАН РИЛСКИ”, Том 49, Св. I, Геология и геофизика, 2006 ANNUAL OF THE UNIVERSITY OF MINING AND GEOLOGY “ST. IVAN RILSKI”, Vol. 49, Part I, Geology and GeopHysics, 2006 SYSTEMATICS AND CRYSTAL GENESIS OF CARBONATE MINERALS Ivan Kostov, Ruslan I. Kostov University of Mining and Geology “St. Ivan Rilski”, Sofia 1700; [email protected] ABSTRACT. A dual crystal structural and paragenetic principle (Kostov, 1993; Kostov, Kostov, 1999) Has been applied to a rational classification of tHe carbonate minerals. Main divisions (associations) are based on geocHemically allied metals in tHe composition of tHese minerals, and subdivisions (axial, planar, pseudoisometric and isometric types) on tHeir overall structural anisometricity. The latter provides botH structural similarity and genetic information, as manner of crystal groWtH in geological setting under different conditions of crystallization. The structural anisometricity may conveniently be presented by tHe c/a ratio of tHe minerals WitH HigH symmetry and by tHe 2c/(a+b), 2b/(a+c) and 2a/(b+c) ratios for tHe loW symmetry minerals. The respective ratios are less, nearly equal, equal or above 1.00. The unit cell or sub-cell and tHe corresponding structures are denoted as axial or A-type, pseudo-isometric or (I)-type, isometric or I-type and planar or P- type, notations WHicH correspond to cHain-like, frameWork and sHeet-like structures, respectively ino-, tecto- and pHyllo-structures. The classification includes tHree geocHemical assemblages among tHe carbonate minerals – Al-Mg-Fe(Ni,Co,Mn), Na-Ca-Ba(К)-REE and Zn-Cu-Pb(U). СИСТЕМАТИКА И КРИСТАЛОГЕНЕЗИС НА КАРБОНАТНИТЕ МИНЕРАЛИ Иван Костов, Руслан И.