Anorthite Porcelain: Synthesis, Phase and Microstructural Evolution
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The Forsterite-Anorthite-Albite System at 5 Kb Pressure Kristen Rahilly
The Forsterite-Anorthite-Albite System at 5 kb Pressure Kristen Rahilly Submitted to the Department of Geosciences of Smith College in partial fulfillment of the requirements for the degree of Bachelor of Arts John B. Brady, Honors Project Advisor Acknowledgements First I would like to thank my advisor John Brady, who patiently taught me all of the experimental techniques for this project. His dedication to advising me through this thesis and throughout my years at Smith has made me strive to be a better geologist. I would like to thank Tony Morse at the University of Massachusetts at Amherst for providing all of the feldspar samples and for his advice on this project. Thank you also to Michael Jercinovic over at UMass for his help with last-minute carbon coating. This project had a number of facets and I got assistance from many different departments at Smith. A big thank you to Greg Young and Dale Renfrow in the Center for Design and Fabrication for patiently helping me prepare and repair the materials needed for experiments. I’m also grateful to Dick Briggs and Judith Wopereis in the Biology Department for all of their help with the SEM and carbon coater. Also, the Engineering Department kindly lent their copy of LabView software for this project. I appreciated the advice from Mike Vollinger within the Geosciences Department as well as his dedication to driving my last three samples over to UMass to be carbon coated. The Smith Tomlinson Fund provided financial support. Finally, I need to thank my family for their support and encouragement as well as my friends here at Smith for keeping this year fun and for keeping me balanced. -
The Surface Reactions of Silicate Minerals
RESEARCH BULLETIN 614 SEPTEMBER, 1956 UNIVERSITY OF MISSOURI COLLEGE OF AGRICULTURE AGRICULTURAL EXPERIMENT STATION J. H. Longwell, Director The Surface Reactions Of Silicate Minerals PART II. REACTIONS OF FELDSPAR SURFACES WITH SALT SOLUTIONS. V. E. NASH AND C. E. MARSHALL (Publication authorized September 5, 1956) COLUMBIA, MISSOURI TABLE OF CONTENTS Introduction .......... .. 3 The Interaction of Albite with Salt Solutions . .. 4 The Interaction of Anorthite with Salt Solutions ........ .. 7 Relative Effectiveness of Ammonium Chloride and Magnesium Chloride on the Release of Sodium from Albite . .. 9 Surface Interaction of Albite with Salt Solutions in Methanol . .. 13 Experiments on Cationic Fixation ............................... 16 Detailed Exchange and Activity Studies with Individual Feldspars .......... .. 19 Procedure .. .. 20 Microcline . .. 21 Albite .................................................... 22 Oligoclase . .. 23 Andesine . .. 24 Labradori te . .. 25 Bytownite ................................................. 25 Anorthite . .. 27 Discussion ........ .. 28 Summary ..................................................... 35 References .. .. 36 Most of the experimental material of this and the preceding Research Bulletin is taken from the Ph.D. Thesis of Victor Nash, University of Missouri, June 1955. The experiments on cation fixation were carried our with the aid of a research grant from the Potash Rock Company of America, Lithonia, Georgia, for which the authors wish to record their appreciation. The work was part of Department of Soils Research Project No.6, entitled, "Heavy Clays." The Surface Reactions of Silicate Minerals PART II. REACTIONS OF FELDSPAR SURFACES WITH SALT SOLUTIONS. v. E. NASH AND C. E. MARSHALL INTRODUCTION The review of literature cited in Part I of this series indicates that little is known of the interaction of feldspar surfaces with salt solutions. The work of Breazeale and Magistad (1) clearly demonstrated that ex change reactions between potassium and calcium occur in the case of or thoclase surfaces. -
Noritic Anorthosite Bodies in the Sierra Nevada Batholith
MINERALOGICAL SOCIETY OF AMERICA, SPECIAL PAPER 1, 1963 INTERNATIONALMINERALOGICAL ASSOCIATION,PAPERS, THIRD GENERAL MEETING NORITIC ANORTHOSITE BODIES IN THE SIERRA NEVADA BATHOLITH ALDEN A. LOOMISl Department of Geology, Stanford University, Stanford, California ABSTRACT A group of small noritic plutons were intruded prior to the immediately surrounding granitic rocks in a part of the composite Sierra Nevada batholith near Lake Tahoe. Iron was more strongly concentrated in the late fluids of individual bodies than during the intrusive sequence as a whole. Pyroxenes are more ferrous in rocks late in the sequence, although most of the iron is in late magnetite which replaces pyroxenes. Both Willow Lake type and normal cumulative layering are present. Cumulative layering is rare; Willi ow Lake layering is common and was formed early in individual bodies. Willow Lake layers require a compositional uniqueness providing high ionic mobility to explain observed relations. The Sierran norites differ from those in large stratiform plutons in that (1) the average bulk composition is neritic anorthosite in which typical rocks contain over 20% AbO" and (2) differentiation of both orthopyroxene and plagioclase produced a smooth progressive sequence of mineral compositions. A plot of modal An vs. En for all the rocks in the sequence from early Willow Lake-type layers to late no rite dikes defines a smooth non-linear trend from Anss-En76 to An,,-En54. TLe ratio An/ Ab decreased faster than En/Of until the assemblage Anso-En65 was reached and En/Of began to decrease more rapidly. Similar plots for large stratiform bodies show too much scatter to define single curves. -
Fluid Inclusions Confirm Authenticity of Tibetan Andesine Date
GEMOLOGY Fluid Inclusions Confirm Authenticity of Tibetan Andesine Can Tibetan andesine now be certified? By Adolf Peretti1, Willy Bieri1, Kathrin Hametner2 and Detlef Günther2 with Richard W. Hughes and Ahmadjan Abduriyim Introduction Untreated copper-bearing feldspar of a rich red color is found in nature, but gem-quality pieces are scarce. For decades the major occurrence has been in Oregon (USA), but gem-quality red feld- spar also occurs in Japan (Furuya & Milisenda, 2009) and elsewhere. Beginning in 2002, gem-quality red plagioclase feldspar en- tered world gem markets. The source was originally stated as the Congo and later morphed into Tibet. By 2007, suspicions that such stones were the result of a treatment were widespread. These suspicions were confirmed in early 2008 (Furuya, 2008), when the treatment was revealed as one of copper diffusion into otherwise lightly-colored plagioclase. This was confirmed by laboratory experiments which replicated the treatment (Emmett & Douthit, 2009). Still, the question remained. Was there a genuine red feldspar mine in Tibet? If so, how would one separate such stones from the treated material? This question challenged the gemological community, resulting in several expeditions to the alleged Tibet- an localities for sample collection and subsequent testing. Figure 2. Copper-bearing red collected by Abduriyim from Yu Lin Gu and view into the valley. (Photos: Ahmadjan Abduriyim) The first of these forays was in 2008 to Bainang, southeast of Shigatse. A group led by Ahmadjan Abduriyim collected numer- ous samples and found the deposit to be credible. However, two subsequent visits (to two widely separated deposits, one of which was adjacent to Bainang) suggested copper-bearing an- desine occurrences in Tibet were being “salted” (Fontaine et al., 2010; Wang et al., 2010). -
Constraining the Source Regions of Lunar Meteorites Using Orbital Geochemical Data
Meteoritics & Planetary Science 50, Nr 2, 214–228 (2015) doi: 10.1111/maps.12412 Constraining the source regions of lunar meteorites using orbital geochemical data A. CALZADA-DIAZ1,2*, K. H. JOY3, I. A. CRAWFORD1,2, and T. A. NORDHEIM2,4 1Department of Earth and Planetary Sciences, Birkbeck College, London WC1E 7HX, UK 2Centre for Planetary Sciences UCL/Birkbeck, London WC1E 6BT, UK 3School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK 4Mullard Space Science Laboratory, University College London, Dorking RH5 6NT, UK *Corresponding author. E-mail: [email protected] (Received 30 July 2014; revision accepted 06 November 2014) Abstract–Lunar meteorites provide important new samples of the Moon remote from regions visited by the Apollo and Luna sample return missions. Petrologic and geochemical analysis of these meteorites, combined with orbital remote sensing measurements, have enabled additional discoveries about the composition and age of the lunar surface on a global scale. However, the interpretation of these samples is limited by the fact that we do not know the source region of any individual lunar meteorite. Here, we investigate the link between meteorite and source region on the Moon using the Lunar Prospector gamma ray spectrometer remote sensing data set for the elements Fe, Ti, and Th. The approach has been validated using Apollo and Luna bulk regolith samples, and we have applied it to 48 meteorites excluding paired stones. Our approach is able broadly to differentiate the best compositional matches as potential regions of origin for the various classes of lunar meteorites. Basaltic and intermediate Fe regolith breccia meteorites are found to have the best constrained potential launch sites, with some impact breccias and pristine mare basalts also having reasonably well-defined potential source regions. -
Norwegian Anorthosites and Their Industrial Uses, with Emphasis on the Massifs of the Inner Sogn-Voss Area in Western Norway
NGU-BULL 436, 2000 - PAGE 103 Norwegian anorthosites and their industrial uses, with emphasis on the massifs of the Inner Sogn-Voss area in western Norway JAN EGIL WANVIK Wanvik, J.E. 2000: Norwegian anorthosites and their industrial uses, with emphasis on the massifs of the Inner Sogn- Voss area in western Norway. Norges geologiske undersøkelse Bulletin 436, 103-112. Anorthositic rocks are common in several geological provinces in Norway. Many occur at scattered localities in different parts of the country, but the two largest anorthosite complexes in western Europe are situated in western Norway. These two Precambrian massifs, the Inner Sogn-Voss province (~ 1700 Ma), and the Rogaland province (~ 930 Ma) have been investigated for use as a raw material for various industrial applications. Anorthosite with a high anorthite content (An >70) is easily soluble in mineral acids, and the bytownite plagioclase of the Sogn anorthosite makes it well suited for industrial processes based on acid leaching. The high aluminium content, ca. 31% Al2O3, has made these occurrences interesting for various industrial applications, especially as an alternative raw material for the Norwegian aluminium industry. With this goal in mind, geological investigations and processing studies have been carried out at various times during the past century. At present, a refined process utilising both the silicon and the calcium contents of the anorthosite has renewed industrial interest in these acid soluble anorthosites. Jan Egil Wanvik, Geological Survey of Norway, N-7491 Trondheim, Norway. Introduction Anorthositic rocks are common in several geological prov- inces in Norway and occur at many localities in different parts of the country (Fig. -
A Database of Plagioclase Crystal Preferred Orientations (CPO)
Solid Earth, 4, 511–542, 2013 Open Access www.solid-earth.net/4/511/2013/ doi:10.5194/se-4-511-2013 Solid Earth © Author(s) 2013. CC Attribution 3.0 License. A database of plagioclase crystal preferred orientations (CPO) and microstructures – implications for CPO origin, strength, symmetry and seismic anisotropy in gabbroic rocks T. Satsukawa1,2,*, B. Ildefonse2, D. Mainprice2, L. F. G. Morales3, K. Michibayashi1,4, and F. Barou2 1Graduate School of Science and Technology, Shizuoka University, Ohya 836, Shizuoka 422-8529, Japan 2Géosciences Montpellier, Université Montpellier 2 and CNRS, CC 060, 34095 Montpellier cedex 5, France 3Helmholtz Zentrum Potsdam, Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany 4Institute of Geosciences, Shizuoka University, Ohya 836, Shizuoka 422-8529, Japan *present address: ARC Center of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia Correspondence to: T. Satsukawa ([email protected]) Received: 3 August 2013 – Published in Solid Earth Discuss.: 14 August 2013 Revised: 14 November 2013 – Accepted: 19 November 2013 – Published: 18 December 2013 Abstract. This study presents a unique database of 172 pla- ture compared with magmatic flow, and the large number gioclase Crystallographic Preferred Orientations (CPO) of of possible slip-systems in plagioclase probably account for variously deformed gabbroic rocks. The CPO characteris- these differences. Calculated seismic properties (P wave and tics as a function of the deformation regime (magmatic or S wave velocities and anisotropies) of plagioclase aggregates crystal-plastic) are outlined and discussed. The studied sam- show that anisotropy (up to 12 % for P wave and 14 % for ples are dominantly from slow- and fast-spread present-day S wave) tends to increase as a function of ODF J index. -
Mineralogy and Origin of the Titanium
MINERALOGY AND ORIGIN OF THE TITANIUM DEPOSIT AT PLUMA HIDALGO, OAXACA, MEXICO by EDWIN G. PAULSON S. B., Massachusetts Institute of Technology (1961) SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY May 18, 1962 Signature of At r . Depardnent of loggand Geophysics, May 18, 1962 Certified by Thesis Supervisor Ab Accepted by ...... Chairman, Departmental Committee on Graduate Students M Abstract Mineralogy and Origin of the Titanium Deposit at Pluma Hidalgo, Oaxaca, Mexico by Edwin G. Paulson "Submitted to the Department of Geology and Geophysics on May 18, 1962 in partial fulfillment of the requirements for the degree of Master of Science." The Pluma Hidalgo titanium deposits are located in the southern part of the State of Oaxaca, Mexico, in an area noted for its rugged terrain, dense vegetation and high rainfall. Little is known of the general and structural geology of the region. The country rocks in the area are a series of gneisses containing quartz, feldspar, and ferromagnesians as the dominant minerals. These gneisses bear some resemblance to granulites as described in the literature. Titanium minerals, ilmenite and rutile, occur as disseminated crystals in the country rock, which seems to grade into more massive and large replacement bodies, in places controlled by faulting and fracturing. Propylitization is the main type of alteration. The mineralogy of the area is considered in some detail. It is remarkably similar to that found at the Nelson County, Virginia, titanium deposits. The main minerals are oligoclase - andesine antiperthite, oligoclase- andesine, microcline, quartz, augite, amphibole, chlorite, sericite, clinozoi- site, ilmenite, rutile, and apatite. -
Ab Initio Calculations of Elastic Constants of Plagioclase Feldspars
UC Berkeley UC Berkeley Previously Published Works Title Ab initio calculations of elastic constants of plagioclase feldspars Permalink https://escholarship.org/uc/item/9fg3d711 Journal American Mineralogist, 99(11-12) ISSN 0003-004X Authors Kaercher, P Militzer, B Wenk, HR Publication Date 2014-11-01 DOI 10.2138/am-2014-4796 Peer reviewed eScholarship.org Powered by the California Digital Library University of California American Mineralogist, Volume 99, pages 2344–2352, 2014 Ab initio calculations of elastic constants of plagioclase feldspars PAMELA KAERCHER1,*, BURKHARD MILITZER1,2 AND HANS-RUDOLF WENK1 1Department of Earth and Planetary Science, University of California, Berkeley, California 94720, U.S.A. 2Department of Astronomy, University of California, Berkeley, California 94720, U.S.A. ABSTRACT Plagioclase feldspars comprise a large portion of the Earth’s crust and are very anisotropic, mak- ing accurate knowledge of their elastic properties important for understanding the crust’s anisotropic seismic signature. However, except for albite, existing elastic constants for plagioclase feldspars are derived from measurements that cannot resolve the triclinic symmetry. We calculate elastic constants for plagioclase end-members albite NaAlSi3O8 and anorthite CaAl2Si2O8 and intermediate andesine/ labradorite NaCaAl3Si5O16 using density functional theory to compare with and improve existing elastic constants and to study trends in elasticity with changing composition. We obtain elastic con- stants similar to measured elastic constants and find that anisotropy decreases with anorthite content. Keywords: Plagioclase feldspars, elastic constants, ab initio calculations, seismic anisotropy INTRODUCTION and taken into account. Plagioclase feldspars are one of the most important rock- Further uncertainty is introduced when elastic constants are forming minerals, comprising roughly 40% of the Earth’s crust. -
An Investigation Into the UV Fluorescence of Feldspar Group
An Investigation into UV Fluorescence in Feldspar Group Minerals Natasha Morrison Submitted in Partial Fulfillment of the Requirement for the Degree of Honours Bachelor of Science, Department of Earth Sciences At Dalhousie University Halifax, Nova Scotia March 17th, 2013 Submitted to: Dr. Richard Cox Dr. Martin Gibling 1 Distribution License DalSpace requires agreement to this non-exclusive distribution license before your item can appear on DalSpace. NON-EXCLUSIVE DISTRIBUTION LICENSE You (the author(s) or copyright owner) grant to Dalhousie University the non-exclusive right to reproduce and distribute your submission worldwide in any medium. You agree that Dalhousie University may, without changing the content, reformat the submission for the purpose of preservation. You also agree that Dalhousie University may keep more than one copy of this submission for purposes of security, back-up and preservation. You agree that the submission is your original work, and that you have the right to grant the rights contained in this license. You also agree that your submission does not, to the best of your knowledge, infringe upon anyone's copyright. If the submission contains material for which you do not hold copyright, you agree that you have obtained the unrestricted permission of the copyright owner to grant Dalhousie University the rights required by this license, and that such third-party owned material is clearly identified and acknowledged within the text or content of the submission. If the submission is based upon work that has been sponsored or supported by an agency or organization other than Dalhousie University, you assert that you have fulfilled any right of review or other obligations required by such contract or agreement. -
Optical Properties of Common Rock-Forming Minerals
AppendixA __________ Optical Properties of Common Rock-Forming Minerals 325 Optical Properties of Common Rock-Forming Minerals J. B. Lyons, S. A. Morse, and R. E. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig. 13-3. A. High Positive Relief Zircon ZrSiO. Tet. (+) 111=1.940 High biref. Small euhedral grains show (.055) parallel" extinction; may cause pleochroic haloes if enclosed in other minerals Sphene CaTiSiOs Mon. (110) (+) 30-50 13=1.895 High biref. Wedge-shaped grains; may (Titanite) to 1.935 (0.108-.135) show (110) cleavage or (100) Often or (221) parting; ZI\c=51 0; brownish in very high relief; r>v extreme. color CtJI\) 0) Gamet AsB2(SiO.la where Iso. High Grandite often Very pale pink commonest A = R2+ and B = RS + 1.7-1.9 weakly color; inclusions common. birefracting. Indices vary widely with composition. Crystals often euhedraL Uvarovite green, very rare. Staurolite H2FeAI.Si2O'2 Orth. (010) (+) 2V = 87 13=1.750 Low biref. Pleochroic colorless to golden (approximately) (.012) yellow; one good cleavage; twins cruciform or oblique; metamorphic. Olivine Series Mg2SiO. Orth. (+) 2V=85 13=1.651 High biref. Colorless (Fo) to yellow or pale to to (.035) brown (Fa); high relief. Fe2SiO. Orth. (-) 2V=47 13=1.865 High biref. Shagreen (mottled) surface; (.051) often cracked and altered to %II - serpentine. Poor (010) and (100) cleavages. Extinction par- ~ ~ alleL" l~4~ Tourmaline Na(Mg,Fe,Mn,Li,Alk Hex. (-) 111=1.636 Mod. biref. -
The Origin of Formation of the Amphibolite- Granulite Transition
The Origin of Formation of the Amphibolite- Granulite Transition Facies by Gregory o. Carpenter Advisor: Dr. M. Barton May 28, 1987 Table of Contents Page ABSTRACT . 1 QUESTION OF THE TRANSITION FACIES ORIGIN • . 2 DEFINING THE FACIES INVOLVED • • • • • • • • • • 3 Amphibolite Facies • • • • • • • • • • 3 Granulite Facies • • • • • • • • • • • 5 Amphibolite-Granulite Transition Facies 6 CONDITIONS OF FORMATION FOR THE FACIES INVOLVED • • • • • • • • • • • • • • • • • 8 Amphibolite Facies • • • • • • • • 9 Granulite Facies • • • • • • • • • •• 11 Amphibolite-Granulite Transition Facies •• 13 ACTIVITIES OF C02 AND H20 . • • • • • • 1 7 HYPOTHESES OF FORMATION • • • • • • • • •• 19 Deep Crust Model • • • • • • • • • 20 Orogeny Model • • • • • • • • • • • • • 20 The Earth • • • • • • • • • • • • 20 Plate Tectonics ••••••••••• 21 Orogenic Events ••••••••• 22 Continent-Continent Collision •••• 22 Continent-Ocean Collision • • • • 24 CONCLUSION • . • 24 BIBLIOGRAPHY • • . • • • • 26 List of Illustrations Figure 1. Precambrian shields, platform sediments and Phanerozoic fold mountain belts 2. Metamorphic facies placement 3. Temperature and pressure conditions for metamorphic facies 4. Temperature and pressure conditions for metamorphic facies 5. Transformation processes with depth 6. Temperature versus depth of a descending continental plate 7. Cross-section of the earth 8. Cross-section of the earth 9. Collision zones 10. Convection currents Table 1. Metamorphic facies ABSTRACT The origin of formation of the amphibolite granulite transition