Novel Phases in Hetero-Epitaxial and Super-Oxygenated Thin Films of Complex Oxides by Hao Zhang a Thesis Submitted in Conformity
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Ultra-High Pressure Aluminous Titanites in Carbonate-Bearing Eclogites at Shuanghe in Dabieshan, Central China
Ultra-high pressure aluminous titanites in carbonate-bearing eclogites at Shuanghe in Dabieshan, central China D. A. CARSWELL Department of Earth Sciences, University of Sheffield, Sheffield $3 7HF, UK R. N. WILSON Department of Geology, University of Leicester, Leicester LE1 7RH, UK AND M. ZtIAI Institute of Geology, Academia Sinica, P.O. Box 634, Beijing 100029, China Abstract Petrographic features and compositions of titanites in eclogites within the ultra-high pressure metamorphic terrane in central Dabieshan are documented and phase equilibria and thermobarometric implications discussed. Carbonate-bearing eclogite pods in marble at Shuanghe contain primary metamorphic aluminous titanites, with up to 39 mol.% Ca(AI,Fe3+)FSiO4 component. These titanites formed as part of a coesite- bearing eclogite assemblage and thus provide the first direct petrographic evidence that AIFTi_IO_j substitution extends the stability of titanite, relative to futile plus carbonate, to pressures within the coesite stability field. However, it is emphasised that A1 and F contents of such titanites do not provide a simple thermobarometric index of P-T conditions but are constrained by the activity of fluorine, relative to CO2, in metamorphic fluids - as signalled by observations of zoning features in these titanites. These ultra-high pressure titanites show unusual breakdown features developed under more H20-rich amphibolite-facies conditions during exhumation of these rocks. In some samples aluminous titanites have been replaced by ilmenite plus amphibole symplectites, in others by symplectitic intergrowths of secondary, lower AI and F, titanite plus plagioclase. Most other coesite-bearing eclogite samples in the central Dabieshan terrane contain peak assemblage rutile often partly replaced by grain clusters of secondary titanites with customary low AI and F contents. -
Occurrence, Alteration Patterns and Compositional Variation of Perovskite in Kimberlites
975 The Canadian Mineralogist Vol. 38, pp. 975-994 (2000) OCCURRENCE, ALTERATION PATTERNS AND COMPOSITIONAL VARIATION OF PEROVSKITE IN KIMBERLITES ANTON R. CHAKHMOURADIAN§ AND ROGER H. MITCHELL Department of Geology, Lakehead University, 955 Oliver Road, Thunder Bay, Ontario P7B 5E1, Canada ABSTRACT The present work summarizes a detailed investigation of perovskite from a representative collection of kimberlites, including samples from over forty localities worldwide. The most common modes of occurrence of perovskite in archetypal kimberlites are discrete crystals set in a serpentine–calcite mesostasis, and reaction-induced rims on earlier-crystallized oxide minerals (typically ferroan geikielite or magnesian ilmenite). Perovskite precipitates later than macrocrystal spinel (aluminous magnesian chromite), and nearly simultaneously with “reaction” Fe-rich spinel (sensu stricto), and groundmass spinels belonging to the magnesian ulvöspinel – magnetite series. In most cases, perovskite crystallization ceases prior to the resorption of groundmass spinels and formation of the atoll rim. During the final evolutionary stages, perovskite commonly becomes unstable and reacts with a CO2- rich fluid. Alteration of perovskite in kimberlites involves resorption, cation leaching and replacement by late-stage minerals, typically TiO2, ilmenite, titanite and calcite. Replacement reactions are believed to take place at temperatures below 350°C, 2+ P < 2 kbar, and over a wide range of a(Mg ) values. Perovskite from kimberlites approaches the ideal formula CaTiO3, and normally contains less than 7 mol.% of other end-members, primarily lueshite (NaNbO3), loparite (Na0.5Ce0.5TiO3), and CeFeO3. Evolutionary trends exhibited by perovskite from most localities are relatively insignificant and typically involve a decrease in REE and Th contents toward the rim (normal pattern of zonation). -
Anorogenic Alkaline Granites from Northeastern Brazil: Major, Trace, and Rare Earth Elements in Magmatic and Metamorphic Biotite and Na-Ma®C Mineralsq
Journal of Asian Earth Sciences 19 (2001) 375±397 www.elsevier.nl/locate/jseaes Anorogenic alkaline granites from northeastern Brazil: major, trace, and rare earth elements in magmatic and metamorphic biotite and Na-ma®c mineralsq J. Pla Cida,*, L.V.S. Nardia, H. ConceicËaÄob, B. Boninc aCurso de PoÂs-GraduacËaÄo em in GeocieÃncias UFRGS. Campus da Agronomia-Inst. de Geoc., Av. Bento GoncËalves, 9500, 91509-900 CEP RS Brazil bCPGG-PPPG/UFBA. Rua Caetano Moura, 123, Instituto de GeocieÃncias-UFBA, CEP- 40210-350, Salvador-BA Brazil cDepartement des Sciences de la Terre, Laboratoire de PeÂtrographie et Volcanologie-Universite Paris-Sud. Centre d'Orsay, Bat. 504, F-91504, Paris, France Accepted 29 August 2000 Abstract The anorogenic, alkaline silica-oversaturated Serra do Meio suite is located within the Riacho do Pontal fold belt, northeast Brazil. This suite, assumed to be Paleoproterozoic in age, encompasses metaluminous and peralkaline granites which have been deformed during the Neoproterozoic collisional event. Preserved late-magmatic to subsolidus amphiboles belong to the riebeckite±arfvedsonite and riebeckite± winchite solid solutions. Riebeckite±winchite is frequently rimmed by Ti±aegirine. Ti-aegirine cores are strongly enriched in Nb, Y, Hf, and REE, which signi®cantly decrease in concentrations towards the rims. REE patterns of Ti-aegirine are strikingly similar to Ti-pyroxenes from the IlõÂmaussaq peralkaline intrusion. Recrystallisation of mineral assemblages was associated with deformation although some original grains are still preserved. Magmatic annite was converted into magnetite and biotite with lower Fe/(Fe 1 Mg) ratios. Recrystallised amphibole is pure riebeckite. Magmatic Ti±Na-bearing pyroxene was converted to low-Ti aegirine 1 titanite ^ astrophyllite/aenigmatite. -
TRINITY COLLEGE Cambridge Trinity College Cambridge College Trinity Annual Record Annual
2016 TRINITY COLLEGE cambridge trinity college cambridge annual record annual record 2016 Trinity College Cambridge Annual Record 2015–2016 Trinity College Cambridge CB2 1TQ Telephone: 01223 338400 e-mail: [email protected] website: www.trin.cam.ac.uk Contents 5 Editorial 11 Commemoration 12 Chapel Address 15 The Health of the College 18 The Master’s Response on Behalf of the College 25 Alumni Relations & Development 26 Alumni Relations and Associations 37 Dining Privileges 38 Annual Gatherings 39 Alumni Achievements CONTENTS 44 Donations to the College Library 47 College Activities 48 First & Third Trinity Boat Club 53 Field Clubs 71 Students’ Union and Societies 80 College Choir 83 Features 84 Hermes 86 Inside a Pirate’s Cookbook 93 “… Through a Glass Darkly…” 102 Robert Smith, John Harrison, and a College Clock 109 ‘We need to talk about Erskine’ 117 My time as advisor to the BBC’s War and Peace TRINITY ANNUAL RECORD 2016 | 3 123 Fellows, Staff, and Students 124 The Master and Fellows 139 Appointments and Distinctions 141 In Memoriam 155 A Ninetieth Birthday Speech 158 An Eightieth Birthday Speech 167 College Notes 181 The Register 182 In Memoriam 186 Addresses wanted CONTENTS TRINITY ANNUAL RECORD 2016 | 4 Editorial It is with some trepidation that I step into Boyd Hilton’s shoes and take on the editorship of this journal. He managed the transition to ‘glossy’ with flair and panache. As historian of the College and sometime holder of many of its working offices, he also brought a knowledge of its past and an understanding of its mysteries that I am unable to match. -
Perovskite Catio3 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic, Pseudocubic
Perovskite CaTiO3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic, pseudocubic. Point Group: 2/m 2/m 2/m. Commonly resemble distorted cubes, to 12 cm, striated k [001] and [110], rarely cubo-octahedra or octahedra, with additional forms, skeletal, dendritic; reniform, granular massive. Twinning: 90◦and 180◦ about [101], rarely 180◦ about [121], giving complex penetration twins; lamellar and sectored. Physical Properties: Cleavage: {001}, imperfect. Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 5.5 D(meas.) = 3.98–4.26 D(calc.) = 4.02 (synthetic). Optical Properties: Opaque, transparent in thin fragments. Color: Iron-black, brown, reddish brown to yellow; colorless to dark brown in transmitted light; dark bluish gray in reflected light. Streak: White to grayish white. Luster: Adamantine to metallic; may be dull. Optical Class: Biaxial (+); commonly isotropic. Pleochroism: Weak; Z > X. Orientation: X = a; Y = c; Z = b. Dispersion: r> v. n= 2.34–2.37 2V(meas.) = 90◦ R: (400) 19.2, (420) 18.8, (440) 18.4, (460) 18.0, (480) 17.6, (500) 17.3, (520) 17.0, (540) 16.8, (560) 16.6, (580) 16.4, (600) 16.2, (620) 16.1, (640) 16.0, (660) 16.0, (680) 15.9, (700) 15.9 Cell Data: Space Group: P nma (synthetic). a = 5.447(1) b = 7.654(1) c = 5.388(1) Z=4 X-ray Powder Pattern: Synthetic. 2.701 (100), 1.911 (50), 2.719 (40), 1.557 (25), 1.563 (16), 3.824 (14), 1.567 (14) Chemistry: (1) (2) (3) (1) (2) (3) Nb2O5 25.99 FeO 5.69 SiO2 0.33 MgO trace TiO2 58.67 38.70 58.75 CaO 40.69 23.51 41.25 Al2O3 0.82 Na2O 1.72 RE2O3 3.08 K2O 0.44 Total 99.36 100.28 100.00 2+ (1) Val d’Aosta, Italy. -
Strain-Induced Time Reversal Breaking and Half Quantum Vortices Near a Putative Superconducting Tetra-Critical Point in Sr $ 2 $ Ruo $
Strain-induced time reversal breaking and half quantum vortices near a putative superconducting tetra-critical point in Sr2RuO4 Andrew C. Yuan,1 Erez Berg,2 and Steven A. Kivelson1 1Department of Physics, Stanford University, Stanford, CA 93405, USA 2Department of Condensed Matter Physics, Weizmann Institute of Science, Rehovot 7610001, Israel It has been shown [1] that many seemingly contradictory experimental findings concerning the superconducting state in Sr2RuO4 can be accounted for as resulting from the existence of an assumed tetra-critical point at near ambient pressure at which dx2−y2 and gxy(x2−y2) superconducting states are degenerate. We perform both a Landau-Ginzburg and a microscopic mean-field analysis of the effect of spatially varying strain on such a state. In the presence of finite xy shear strain, the superconducting state consists of two possible symmetry-related time-reversal symmetry (TRS) preserving states: d ± g. However, at domain walls between two such regions, TRS can be broken, resulting in a d + ig state. More generally, we find that various natural patterns of spatially varying strain induce a rich variety of superconducting textures, including half-quantum fluxoids. These results may resolve some of the apparent inconsistencies between the theoretical proposal and various experimental observations, including the suggestive evidence of half-quantum vortices [2]. I. INTRODUCTION If it happens that superconducting (SC) orders with two distinct symmetries are comparably fa- vorable for some microscopic reason, it is possible to have a two-parameter phase diagram (e.g. T and isotropic strain, 0) that exhibits a multicriti- cal point (e.g. at = ? and T = T ?) at which the transition temperatures, Tc, of the two different or- (a) (b) ders coincide, as shown in Fig. -
Titanite Ores of the Khibiny Apatite-Nepheline- Deposits: Selective Mining, Processing and Application for Titanosilicate Synthesis
minerals Article Titanite Ores of the Khibiny Apatite-Nepheline- Deposits: Selective Mining, Processing and Application for Titanosilicate Synthesis Lidia G. Gerasimova 1,2, Anatoly I. Nikolaev 1,2,*, Marina V. Maslova 1,2, Ekaterina S. Shchukina 1,2, Gleb O. Samburov 2, Victor N. Yakovenchuk 1 and Gregory Yu. Ivanyuk 1 1 Nanomaterials Research Centre of Kola Science Centre, Russian Academy of Sciences, 14 Fersman Street, Apatity 184209, Russia; [email protected] (L.G.G.); [email protected] (M.V.M.); [email protected] (E.S.S.); [email protected] (V.N.Y.); [email protected] (G.Y.I.) 2 Tananaev Institute of Chemistry of Kola Science Centre, Russian Academy of Sciences, 26a Fersman Street, Apatity 184209, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-815-557-9231 Received: 4 September 2018; Accepted: 10 October 2018; Published: 12 October 2018 Abstract: Geological setting and mineral composition of (apatite)-nepheline-titanite ore from the Khibiny massif enable selective mining of titanite ore, and its processing with sulfuric-acid method, without preliminary concentration in flotation cells. In this process flow diagram, titanite losses are reduced by an order of magnitude in comparison with a conventional flotation technology. Further, dissolution of titanite in concentrated sulfuric acid produces titanyl sulfate, which, in turn, is a precursor for titanosilicate synthesis. In particular, synthetic analogues of the ivanyukite group minerals, SIV, was synthesized with hydrothermal method from the composition based on titanyl-sulfate, and assayed as a selective cation-exchanger for Cs and Sr. -
Natural Titanite Reference Materials for in Situ U‐Pb and Sm‐Nd Isotopic Measurements by LA‐(MC)‐ICP‐MS
Vol. 43 — N° 3 09 p.355– 384 19 Natural Titanite Reference Materials for In Situ U-Pb and Sm-Nd Isotopic Measurements by LA-(MC)-ICP-MS Qian Ma (1, 2),NoreenJ.Evans (3), Xiao-Xiao Ling (2, 4),Jin-HuiYang (2, 4),Fu-YuanWu (2, 4), Zhi-Dan Zhao (1)* and Yue-Heng Yang (2, 4)* (1) State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China (2) State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China (3) School of Earth and Planetary Science, John de Laeter Centre, Curtin University, Perth, WA, Australia (4) Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China * Corresponding authors. e-mails: [email protected] and [email protected] Titanite is a common accessory mineral that preferentially incorporates considerable amounts of U and light rare earth elements in its structure, making it a versatile mineral for in situ U-Pb dating and Sm-Nd isotopic measurement. Here, we present in situ U-Pb ages and Sm-Nd isotope measurement results for four well-known titanite reference materials (Khan, BLR-1, OLT1 and MKED1) and eight titanite crystals that could be considered potential reference material candidates (Ontario, YQ-82, T3, T4, TLS-36, NW-IOA, Pakistan and C253), with ages ranging from ~ 20 Ma to ~ 1840 Ma. Results indicate that BLR-1, OLT1, Ontario, MKED1 and T3 titanite have relatively homogeneous Sm-Nd isotopes and low common Pb and thus can serve as primary reference materials for U-Pb and Sm-Nd microanalysis. -
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 -
Current–Voltage Characteristics of Manganite–Titanite Perovskite Junctions
Current–voltage characteristics of manganite–titanite perovskite junctions Benedikt Ifland1, Patrick Peretzki2, Birte Kressdorf1, Philipp Saring2, Andreas Kelling1, Michael Seibt2 and Christian Jooss*1 Full Research Paper Open Access Address: Beilstein J. Nanotechnol. 2015, 6, 1467–1484. 1Institute of Materials Physics, University of Goettingen, doi:10.3762/bjnano.6.152 Friedrich-Hund-Platz 1, 37077 Goettingen, Germany and 24th Physical Institute, University of Goettingen, Received: 06 March 2015 Friedrich-Hund-Platz 1, 37077 Goettingen, Germany Accepted: 16 June 2015 Published: 07 July 2015 Email: Christian Jooss* - [email protected] This article is part of the Thematic Series "Materials for sustainable energy production, storage, and conversion". * Corresponding author Guest Editor: M. Fichtner Keywords: current–voltage characteristics; perovskites; photovoltaics; polarons © 2015 Ifland et al; licensee Beilstein-Institut. License and terms: see end of document. Abstract After a general introduction into the Shockley theory of current voltage (J–V) characteristics of inorganic and organic semicon- ductor junctions of different bandwidth, we apply the Shockley theory-based, one diode model to a new type of perovskite junc- tions with polaronic charge carriers. In particular, we studied manganite–titanate p–n heterojunctions made of n-doped SrTi1−yNbyO3, y = 0.002 and p-doped Pr1−xCaxMnO3, x = 0.34 having a strongly correlated electron system. The diffusion length of the polaron carriers was analyzed by electron beam-induced current (EBIC) in a thin cross plane lamella of the junction. In the J–V characteristics, the polaronic nature of the charge carriers is exhibited mainly by the temperature dependence of the micro- scopic parameters, such as the hopping mobility of the series resistance and a colossal electro-resistance (CER) effect in the parallel resistance. -
The Propertiesof Anatase Pseudomorphs After
Canadian Mineralogist Vol. 27, pp. 495-498 (1989) THE PROPERTIES OF ANATASE PSEUDOMORPHS AFTER TITANITE ERIC R. VANCE* AND DIANE C. DOERN Atomic Energy of Canada Limited, Whiteshell Nuclear Establishment, Pinawa, Manitoba ROE lLO ABSTRACT The object of the present work was to investigate whether a Ti-rich surface layer tends to protect the Two polycrystalline natural anatase pseudomorphs after titanite against further alteration. This information titanite were studied by scanning electron microscopy, X- is of interest in connection with both the rates of for- ray diffraction and differential thermal and thermogravi- mation of an anatase pseudomorph after titanite, and metric analyses. Millimeter-sized natural crystals of titanite, the long-term leaching of titanite glass-ceramics leached for 30 days in 0.3 or I mol/L HCI in water at (Hayward & Cecchetto 1982, Hayward 1986) 100°C, produced relatively porous pseudomorphs, many of which contain siliceous material and rutile in addition designed for the immobilization of radioactive waste. to anatase. The Ti-rich layer produced in titanite leached in near- neutral ~edia at -90°C is only a few micrometers Keywords: anatase, titanite, pseudomorphs, leaching. thick, even after several months of leaching in the laboratory (Vance 1987). A thicker layer would facili- SOMMAIRE tate the study of protection against leaching, so that anatase pseudomorphs after both natural titanite and Deux echantillons polycristallins d'anatase naturel pro- titanite crystals leached in HCI solutions were exa- duit par Ie remplacement de titanite ont ete etudies en uti- mined. lisant la microscopie electronique a balayage, la diffrac- tion X et des analyses differentielles thermique et thermogravimetrique. -
College Record 2020 the Queen’S College
THE QUEEN’S COLLEGE COLLEGE RECORD 2020 THE QUEEN’S COLLEGE Visitor Meyer, Dirk, MA PhD Leiden The Archbishop of York Papazoglou, Panagiotis, BS Crete, MA PhD Columbia, MA Oxf, habil Paris-Sud Provost Lonsdale, Laura Rosemary, MA Oxf, PhD Birm Craig, Claire Harvey, CBE, MA PhD Camb Beasley, Rebecca Lucy, MA PhD Camb, MA DPhil Oxf, MA Berkeley Crowther, Charles Vollgraff, MA Camb, MA Fellows Cincinnati, MA Oxf, PhD Lond Blair, William John, MA DPhil Oxf, FBA, FSA O’Callaghan, Christopher Anthony, BM BCh Robbins, Peter Alistair, BM BCh MA DPhil Oxf MA DPhil DM Oxf, FRCP Hyman, John, BPhil MA DPhil Oxf Robertson, Ritchie Neil Ninian, MA Edin, MA Nickerson, Richard Bruce, BSc Edin, MA DPhil Oxf, PhD Camb, FBA DPhil Oxf Phalippou, Ludovic Laurent André, BA Davis, John Harry, MA DPhil Oxf Toulouse School of Economics, MA Southern California, PhD INSEAD Taylor, Robert Anthony, MA DPhil Oxf Yassin, Ghassan, BSc MSc PhD Keele Langdale, Jane Alison, CBE, BSc Bath, MA Oxf, PhD Lond, FRS Gardner, Anthony Marshall, BA LLB MA Melbourne, PhD NSW Mellor, Elizabeth Jane Claire, BSc Manc, MA Oxf, PhD R’dg Tammaro, Paolo, Laurea Genoa, PhD Bath Owen, Nicholas James, MA DPhil Oxf Guest, Jennifer Lindsay, BA Yale, MA MPhil PhD Columbia, MA Waseda Rees, Owen Lewis, MA PhD Camb, MA Oxf, ARCO Turnbull, Lindsay Ann, BA Camb, PhD Lond Bamforth, Nicholas Charles, BCL MA Oxf Parkinson, Richard Bruce, BA DPhil Oxf O’Reilly, Keyna Anne Quenby, MA DPhil Oxf Hunt, Katherine Emily, MA Oxf, MRes PhD Birkbeck Louth, Charles Bede, BA PhD Camb, MA DPhil Oxf Hollings, Christopher