THE CHARACTERISTICS and IDENTIFICATION of FILLED DIAMONDS -- by John I, Koivula, Robert C
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Tourmaline Composition of the Kışladağ Porphyry Au Deposit, Western Turkey: Implication of Epithermal Overprint
minerals Article Tourmaline Composition of the Kı¸slada˘gPorphyry Au Deposit, Western Turkey: Implication of Epithermal Overprint Ömer Bozkaya 1,* , Ivan A. Baksheev 2, Nurullah Hanilçi 3, Gülcan Bozkaya 1, Vsevolod Y. Prokofiev 4 , Yücel Özta¸s 5 and David A. Banks 6 1 Department of Geological Engineering, Pamukkale University, 20070 Denizli, Turkey; [email protected] 2 Department of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia; [email protected] 3 Department of Geological Engineering, Istanbul University-Cerrahpa¸sa,Avcılar, 34320 Istanbul, Turkey; [email protected] 4 Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences, 119017 Moscow, Russia; [email protected] 5 TÜPRAG Metal Madencilik, Ovacık Mevki Gümü¸skolKöyü, Ulubey Merkez, 64902 U¸sak,Turkey; [email protected] 6 School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK; [email protected] * Correspondence: [email protected]; Tel.: +90-258-296-3442 Received: 13 August 2020; Accepted: 4 September 2020; Published: 7 September 2020 Abstract: The Kı¸slada˘gporphyry Au deposit occurs in a middle Miocene magmatic complex comprising three different intrusions and magmatic-hydrothermal brecciation related to the multiphase effects of the different intrusions. Tourmaline occurrences are common throughout the deposit, mostly as an outer alteration rim around the veins with lesser amounts disseminated in the intrusions, and are associated with every phase of mineralization. Tourmaline mineralization has developed as a tourmaline-rich matrix in brecciated zones and tourmaline-quartz and/or tourmaline-sulfide veinlets within the different intrusive rocks. Tourmaline was identified in the tourmaline-bearing breccia zone (TBZ) and intrusive rocks that had undergone potassic, phyllic, and advanced argillic alteration. -
Structural Geology of the Upper Rock Creek Area, Inyo County, California, and Its Relation to the Regional Structure of the Sierra Nevada
Structural geology of the upper Rock Creek area, Inyo County, California, and its relation to the regional structure of the Sierra Nevada Item Type text; Dissertation-Reproduction (electronic); maps Authors Trent, D. D. 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 27/09/2021 06:38:23 Link to Item http://hdl.handle.net/10150/565293 STRUCTURAL GEOLOGY OF THE UPPER ROCK CREEK AREA, INYO COUNTY, CALIFORNIA, AND ITS RELATION TO THE REGIONAL STRUCTURE OF THE SIERRA NEVADA by Dee Dexter Trent 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 1 9 7 3 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE I hereby recommend that this dissertation prepared under my direction by __________ Dee Dexter Trent______________________ entitled Structural Geology of the Upper Rock Creek Area . Tnvo County, California, and Its Relation to the Regional Structure of the Sierra Nevada ________________ be accepted as fulfilling the dissertation requirement of the degree of ____________Doctor of Philosophy_________ ___________ P). /in /'-/7. 3 Dissertation Director fJ Date After inspection of the final copy of the dissertation, the following members of the Final Examination Committee concur in its approval and recommend its acceptance:* f t M m /q 2 g ££2 3 This approval and acceptance is contingent on the candidate's adequate performance and defense of this dissertation at the final oral examination. -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Microstructural, Mechanical, Corrosion and Cytotoxicity Characterization of Porous Ti-Si Alloys with Pore-Forming Agent
materials Article Microstructural, Mechanical, Corrosion and Cytotoxicity Characterization of Porous Ti-Si Alloys with Pore-Forming Agent Andrea Školáková 1,*, Jana Körberová 1 , Jaroslav Málek 2 , Dana Rohanová 3, Eva Jablonská 4, Jan Pinc 1, Pavel Salvetr 1 , Eva Gregorová 3 and Pavel Novák 1 1 Department of Metals and Corrosion Engineering, University of Chemistry and Technology Prague, Technická 5, 166 28 Prague 6, Czech Republic; [email protected] (J.K.); [email protected] (J.P.); [email protected] (P.S.); [email protected] (P.N.) 2 UJP Praha a.s., Nad Kamínkou 1345, 156 10 Prague 16, Czech Republic; [email protected] 3 Department of Glass and Ceramics, University of Chemistry and Technology Prague, Technická 5, 166 28 Prague 6, Czech Republic; [email protected] (D.R.); [email protected] (E.G.) 4 Department of Biochemistry and Microbiology, University of Chemistry and Technology Prague, Technická 5, 166 28 Prague 6, Czech Republic; [email protected] * Correspondence: [email protected]; Tel.: +420-220-444-055 Received: 12 November 2020; Accepted: 7 December 2020; Published: 9 December 2020 Abstract: Titanium and its alloys belong to the group of materials used in implantology due to their biocompatibility, outstanding corrosion resistance and good mechanical properties. However, the value of Young’s modulus is too high in comparison with the human bone, which could result in the failure of implants. This problem can be overcome by creating pores in the materials, which, moreover, improves the osseointegration. Therefore, TiSi2 and TiSi2 with 20 wt.% of the pore-forming agent (PA) were prepared by reactive sintering and compared with pure titanium and titanium with the addition of various PA content in this study. -
Lessons from Tourmaline-Quartz Intergrowths
Goldschmidt2020 Abstract Inclusion trapping during disequilibrium pegmatite crystallization: lessons from tourmaline-quartz intergrowths MONA-LIZA C. SIRBESCU1*, NIELS HULSBOSCH2 1Central Michigan Univ., Mount Pleasant, MI, USA (*correspondence: [email protected]) 2KU Leuven Univ., Leuven, Belgium Tourmaline-quartz intergrowths (QTI’s) occur in rapidly cooled wall zones of granitic pegmatites (e.g., Black Hills, South Dakota; Oxford Co., Maine; San Diego, California, etc.). This poorly studied skeletal, disequilibrium texture may hold clues about the magmatic evolution and potential development of diffusion-controlled boundary layers and localized fluid saturation at early magmatic stage of crystallization. Unlike graphic quartz-feldspar, tourmaline hosts well preserved crystallized melt inclusion (MI’s) and fluid inclusions (FI’s). Tourmaline tapered habit indicates direction of growth, whereas its color zones allow sequence “stratigraphy” interpretations of inclusion assemblages. Comb-textured, radiating schorl-dravite to foitite tourmaline crystals (<0.5 m long) nucleated in the hanging wall of Emmons pegmatite, Maine and developed remarkable QTI’s comprised of optically coherent central tourmaline prisms and skeletal “branches” intergrown with coarse, anhedral quartz. Crystallized MI’s were mapped through high-resolution, confocal Raman spectroscopy, using 3D imagining and multivariate spectral fitting. We integrated full-spectrum mixture analysis and database matching to separate the daughter-mineral and host-tourmaline spectra. Primary crystallized MI’s in the rims of central tourmaline contain quartz (~45% by area); peraluminous phases muscovite (~30%), pyrophyllite (0-5%), and garnet (<2%); and aqueous- carbonic fluid (15-25%). Carbonates and phosphates (5-10%) demonstrate progressive flux-component enrichment at the transition between subhedral to skeletal growth. Moreover, the fluid content in the MI’s and the abundance of primary, aqueous-carbonic FI’s increase in the skeletal zone. -
On Palaeozoic–Mesozoic Brittle Normal Faults Along the SW Barents Sea Margin: Fault Processes and Implications for Basement Permeability and Margin Evolution
research-articleResearch ArticleXXX10.1144/jgs2014-018K. Indrevær et al.Brittle Faults on the SW Barents Sea Margin 2014 Downloaded from http://jgs.lyellcollection.org/ by guest on October 9, 2021 Journal of the Geological Society, London. http://dx.doi.org/10.1144/jgs2014-018 Published Online First © 2014 The Authors On Palaeozoic–Mesozoic brittle normal faults along the SW Barents Sea margin: fault processes and implications for basement permeability and margin evolution KJETIL INDREVÆR1,2*, HOLGER STUNITZ1 & STEFFEN G. BERGH1 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway 2DONG E&P Norge AS, Roald Amundsens Plass 1, N-9257 Tromsø, Norway *Corresponding author (e-mail: [email protected]) Abstract: Palaeozoic–Mesozoic brittle normal faults onshore along the SW Barents Sea passive margin off northern Norway give valuable insight into fault and fluid flow processes from the lower brittle crust. Micro- structural evidence suggests that Late Permian–Early Triassic faulting took place during multiple phases, with initial fault movement at minimum P–T conditions of c. 300 °C and c. 240 MPa (c. 10 km depth), followed by later fault movement at minimum P–T conditions of c. 275 °C and c. 220 MPa (c. 8.5 km depth). The study shows that pore pressures locally reached lithostatic levels (240 MPa) during faulting and that faulting came to a halt during early (deep) stages of rifting along the margin. Fault permeability has been controlled by heal- ing and precipitation processes through time, which have sealed off the core zone and eventually the damage zones after faulting. A minimum average exhumation rate of c. -
Experimental and Computational Study of Fracturing in an Anisotropic Brittle Solid
Mechanics of Materials 28Ž. 1998 247±262 Experimental and computational study of fracturing in an anisotropic brittle solid Abbas Azhdari 1, Sia Nemat-Nasser ) Center of Excellence for AdÕanced Materials, Department of Applied Mechanics and Engineering Sciences, UniÕersity of California-San Diego, La Jolla, CA 92093-0416, USA Received 21 November 1996; revised 26 August 1997 Abstract For isotropic materials, stress- and energy-based fracture criteria lead to fairly similar results. Theoretical studies show that the crack-path predictions made by these criteria are not identical in the presence of strong material anisotropy. Therefore, experiments are performed to ascertain which criterion may apply to anisotropic materials. Notched specimens made from sapphire, a microscopically homogeneous and brittle solid, are used for the experiments. An attempt is made to locate the notch on different crystallographic planes and thus to examine the fracture path along different cleavage planes. The experimental observations are compared with the numerical results of the maximum tensile stress and the maximum energy-release rate criteria. It is observed that most of the notched specimens are fractured where the tensile stress is maximum, whereas the energy criterion fails to predict the fracture path of most of the specimens. For the tensile-stress Žn. s p s r g s fracture criterion, a dimensionless parameter, A ''2 R0 nn a Enn, is introduced, where nnand E nn, respectively, are the tensile stress and Young's modulus in the direction normal to the cleavage plane specified by the angle a Žthe fracture surface energy of this plane is ga . and R0 is a characteristic length, e.g. -
Activity 21: Cleavage and Fracture Maine Geological Survey
Activity 21: Cleavage and Fracture Maine Geological Survey Objectives: Students will recognize the difference between cleavage and fracture; they will become familiar with planes of cleavage, and will use a mineral's "habit of breaking" as an aid to identifying common minerals. Time: This activity is intended to take one-half (1/2) period to discuss cleavage planes and types and one (1) class period to do the activity. Background: Cleavage is the property of a mineral that allows it to break smoothly along specific internal planes (called cleavage planes) when the mineral is struck sharply with a hammer. Fracture is the property of a mineral breaking in a more or less random pattern with no smooth planar surfaces. Since nearly all minerals have an orderly atomic structure, individual mineral grains have internal axes of length, width, and depth, related to the consistent arrangement of the atoms. These axes are reflected in the crystalline pattern in which the mineral grows and are present in the mineral regardless of whether or not the sample shows external crystal faces. The axes' arrangement, size, and the angles at which these axes intersect, all help determine, along with the strength of the molecular bonding in the given mineral, the degree of cleavage the mineral will exhibit. Many minerals, when struck sharply with a hammer, will break smoothly along one or more of these planes. The degree of smoothness of the broken surface and the number of planes along which the mineral breaks are used to describe the cleavage. The possibilities include the following. Number of Planes Degree of Smoothness One Two Three Perfect Good Poor Thus a mineral's cleavage may be described as perfect three plane cleavage, in which case the mineral breaks with almost mirror-like surfaces along the three dimensional axes; the mineral calcite exhibits such cleavage. -
Correlation of the Mohs's Scale of Hardness with the Vickers' S Hardness Numbers
718 Correlation of the Mohs's scale of hardness with the Vickers' s hardness numbers. By E. WILFRED TAYLOR, C.B.E., F.R.M.S., F. Inst. P. Messrs. Cooke, Troughton & Simms, Ltd., York. [Read June 23, 1949.] INERALOGISTS have long been accustomed to describe hard- M ness with the aid of a scale devised by Friedrich Mohs, who lived from 1773 to 1839. The test is qualitative, each mineral in the scale being capable of scratching those that precede it, but the ten minerals have held their ground as a useful representative series with which it is now interesting to compare another method of estimating hard- ness. In the metallurgical world hardness is now usually expressed by means of the Vickers's hardness numbers or their equivalent, and the figures are derived from the size of the impression made by a diamond indenter in the form of a four-sided pyramid with the opposite faces worked to an included angle of 136 ~ More recently micro-hardness testers have been devised to enable minute impressions to be formed under light loads on small individual crystals of a metallic alloy, 1 and it occurred to the author to obtain hardness figures for the various types of optical glass by means of a scratch test with such an instrument. The intention was to draw a lightly loaded diamond across a polished glass surface and to measure the width of the resulting furrow. This method proved to be promising, but as an experiment a static indenter was also used, and it was dis- covered that glass was sufficiently plastic to take good impressions, so long as the load did not exceed 50 grams or thereabouts. -
Fluid-Inclusion Petrology Data from Porphyry Copper Deposits and Applications to Exploration COVER PHOTOGRAPHS 1
- . Fluid-Inclusion Petrology Data from PorpHyry Copper Deposits and Applications to Exploration COVER PHOTOGRAPHS 1. Asbestos ore 8. Aluminum ore, bauxite, Georgia I 2 3 4 2. Lead ore, Balmat mine, N.Y. 9. Native copper ore, Keweenawan 5 6 3. Chromite, chromium ore, Washington Peninsula, Mich. 4. Zinc ore, Friedensville, Pa. 10. Porphyry molybdenum ore, Colorado 7 8 5. Banded iron-formation, Palmer, 11. Zinc ore, Edwards, N.Y. Mich. 12. Manganese nodules, ocean floor 9 10 6. Ribbon asbestos ore, Quebec, Canada 13. Botryoidal fluorite ore, 7. Manganese ore, banded Poncha Springs, Colo. II 12 13 14 rhodochrosite 14. Tungsten ore, North Carolina Fluid-Inclusion Petrology Data from Porphyry Copper Deposits and Applications to Exploration By]. THOMAS NASH GEOLOGY AND RESOURCES OF COPPER DEPOSITS GEOLOGICAL SURVEY PROFESSIONAL PAPER 907-D A summary of new and published descriptions offluid inclusions from 3 6 porphyry copper deposits and discussion of possible applica'tions to exploration for copper deposits 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 Nash, John Thomas, 1941- Fluid-inclusion petrology-data from porphyry copper deposits and applications to exploration. (Geology and Resources of Copper Deposits) (Geological Survey Professional Paper 907-D) Bibliography: p. Supt. of Docs. no.: I 19.16:907-D 1. Porphyry-Inclusions. 2. Porphyry-Southwestern States. 3. Copper ores-Southwestern States. I. Title. II. Series. III. Series: United States Geological Survey Professional Paper 907-D. QE462.P6N37 549'.23 76-608145 For sale by the Superintendent of Documents, U.S. -
Non-Stoichiometric Magnesium Aluminate Spinel
NON-STOICHIOMETRIC MAGNESIUM ALUMINATE SPINEL: MICROSTRUCTURE EVOLUTION AND ITS EFFECT ON PROPERTIES by J. Aaron Miller A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Materials Science). Golden, Colorado Date _________________________ Signed: __________________________________ J. Aaron Miller Signed: __________________________________ Ivar E. Reimanis Thesis Advisor Golden, Colorado Date _________________________ Signed: _________________________ Dr. Angus Rockett Professor and Head Department of Metallurgical and Materials Engineering ii ABSTRACT Magnesium aluminate spinel is a material of interest for transparent armor applications. Owing to its unique combination of transparency to large portions of the electromagnetic spectrum and mechanical robustness, spinel is among the front runners for applications including transparent armor windows for military vehicles and space craft windows, missile radomes, and infrared windows. However, failure in such applications may lead to severe outcomes, creating motivation to further improve the mechanical reliability of the materials used. In this thesis, potential toughening mechanisms that utilize unique control over the evolution of second phase particles are explored. Al-rich spinel (MgO•nAl2O3) with a composition of n = 2 is investigated. First, it is demonstrated that precipitation of second phase Al2O3 from single phase spinel can be achieved by modifying the densification