Petrology, Mineralogy, and Geochemistry Northern California
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2009 Medals & Awards Mary C. Rabbitt History of Geology
2009 MEDALS & AWARDS MARY C. RABBITT emeritus since 2004. During his time at But there is more. As he is credited Calvin he was for a year a Fellow at the to be in several web sites, he is a noted HISTORY OF Calvin Center for Christian Scholarship. conservative evangelical Christian who is GEOLOGY AWARD He is a member of GSA, the Mineralogical also a geologist—and is a fine example of Society of America, the American Scientific both. As such, he has access to venues that Presented to Davis A. Young Affiliation, the Affiliation of Christian few of us can address, and is a spokesman Geologists, of which he has been president, for our science with a unique authority. His and the International Commission on the reviews of important books in the history of History of the Geological Sciences. geology speak to a wider audience than many In his long teaching career, I’m sure of us can reach. Dave will tell us more of his Dave has steered many a young person to journey. The Rabbitt Award is most fitting geology, and his department has just instituted recognition of Davis Young. a student Summer Research Fellowship in his name. He co-led a course on Hawaiian geology in the best of places, Hawaii itself. Response by Davis A. Young Reading the program for that, I envy the My profoundest gratitude to the History students who were able to take part in it. With of Geology Division for bestowing this student help, he has also assisted with the honor on me. -
History of Geology
FEBRUARY 2007 PRIMEFACT 563 (REPLACES MINFACT 60) History of geology Mineral Resources Early humans needed a knowledge of simple geology to enable them to select the most suitable rock types both for axe-heads and knives and for the ornamental stones they used in worship. In the Neolithic and Bronze Ages, about 5000 to 2500 BC, flint was mined in the areas which are now Belgium, Sweden, France, Portugal and Britain. While Stone Age cultures persisted in Britain until after 2000 BC, in the Middle East people began to mine useful minerals such as iron ore, tin, clay, gold and copper as early as 4000 BC. Smelting techniques were developed to make the manufacture of metal tools possible. Copper was probably the earliest metal to be smelted, that is, extracted from its ore by melting. Copper is obtained easily by reducing the green copper carbonate mineral malachite, itself regarded as a precious stone. From 4000 BC on, the use of clay for brick-making became widespread. The Reverend William Branwhite Clarke (1798-1878), smelting of iron ore for making of tools and the ‘father’ of geology in New South Wales weapons began in Asia Minor at about 1300 BC but did not become common in Western Europe until Aristotle believed volcanic eruptions and nearly 500 BC. earthquakes were caused by violent winds escaping from the interior of the earth. Since earlier writers had ascribed these phenomena to The classical period supernatural causes, Aristotle's belief was a By recognising important surface processes at marked step forward. Eratosthenes, a librarian at work, the Greek, Arabic and Roman civilisations Alexandria at about 200 BC, made surprisingly contributed to the growth of knowledge about the accurate measurements of the circumference of earth. -
Syllabus: Petrology of Igneous and Metmorphic
Course Syllabus GEOL 333 PETROLOGY OF IGNEOUS AND METAMORPHIC ROCKS Course Description: Study of the properties and genesis of two major rock groups. Megascopic and microscopic techniques in rock classification. Environments of formation. Case studies from the Maryland Piedmont. Field trips required. Six contact hours (three lecture hours and three laboratory hours), four credits. Prerequisite: GEOL 331. Schedule of lecture and laboratory topics: subject to change with notice: WEEK MONDAY: Laboratory Topic WEDNESDAY: Lecture/Lab Topic TEXT Types of Intrusions; Composition, Introduction to Course; Igneous 1/30-2/1 Textures & Structures of Igneous 1–3 Rocks in Hand Sample Rocks; Classification Volcanism; Formation of Magma; 2/6-8 Igneous Textures in Thin Section 4–6 Crystallization of Magma Igneous Rocks of the Oceanic 2/13-15 Felsic Extrusive Rocks 8 Lithosphere Intermediate and Mafic Extrusive Igneous Rocks of Convergent 2/20-22 9,10 Rocks Margins; Layered Mafic Intrusions 2/27-29 Felsic Intrusive Rocks Mafic Intrusive Rocks 3/5-7 Work on Igneous Case Study Ellicott City Field Trip 3/12-14 Work on Igneous Case Study Igneous Case Study due 3/19-21 SPRING BREAK Metamorphic Isograds, Facies, P-T 3/26-28 Quartz Microstructures Evolution; Metamorphic Textures and 17,18 Classification Metamorphic Assemblages, 4/2-4 Metamorphic Index Minerals 19-20 Reactions, and Equilibrium Metamorphism of Mafic & 4/9-11 Foliated Metamorphic Rocks 21 Ultramafic Rocks Metamorphism of Aluminous Clastic 4/16-18 Non-foliated Metamorphic Rocks 22 Rocks 4/23-26 Determining P-T-t Histories Maryland Piedmont: Lang articles 4/30-5/2 Work on Piedmont Project Hunt Valley Field Trip 5/7-9 Work on Piedmont Project Work on Piedmont Project 5/14 Present Piedmont Project Piedmont Project due Friday, May 18th, 8:00 – 10:00 a.m. -
Single Crystal Growth for Topology and Beyond Chandra Shekhar#, Horst Borrmann, Claudia Felser, Guido Kreiner, Kaustuv Manna, Marcus Schmidt, and Vicky Sü
CHEMICAL METALS SCIENCE & SOLID STATE CHEMISTRY Single crystal growth for topology and beyond Chandra Shekhar#, Horst Borrmann, Claudia Felser, Guido Kreiner, Kaustuv Manna, Marcus Schmidt, and Vicky Sü Single crystals are the pillars for many technological advancements, which begin with acquiring the material. Since different compounds have different physical and chemical properties, different techniques are needed to obtain their single crystals. New classes of quantum materials, from insulators to semimetals, that exhibit non-trivial topologies, have been found. They display a plethora of novel phenomena, including topological surface states, new fermions such as Weyl, Dirac, or Majorana, and non-collinear spin textures such as antiskyrmions. To obtain the crystals and explore the properties of these families of compounds, it is necessary to employ different crystal growth techniques such as the chemical vapour transport method, Bridgman technique, flux growth method, and floating-zone method. For the last four years, we have grown more than 150 compounds in single crystal form by employing these methods. We sometimes go beyond these techniques if the phase diagram of a particular material allows it; e.g., we choose the Bridgman technique as a flux growth method. Before measuring the properties, we fully characterize the grown crystals using different characterization tools. Our TaAs family of crystals have, for the first time, been proven experimentally to exhibit Weyl semimetal properties. They exhibit extremely high magnetoresistance and mobility of charge carriers, which is indicative of the Weyl fermion properties. Moreover, a very large value of intrinsic anomalous Hall and Weyl physics with broken time-reversal symmetry is found in the full-Heuslers, while the half-Heuslers exhibit topological surface states. -
Where Do New Materials Come From? Neither the Stork Nor the Birds and the Bees! in Search of the Next “First Material” Gregory Morrison, Dileka Abeysinghe, Justin B
2016 Governor’s Award for Excellence in Science Where Do New Materials Come From? Neither the Stork nor the Birds and the Bees! In Search of the Next “First Material” Gregory Morrison, Dileka Abeysinghe, Justin B. Felder, Shani Egodawatte, Timothy Ferreira, Hans-Conrad zur Loye* Department of Chemistry and Biochemistry, University of South Carolina, Columbia, South Carolina 29208, USA Materials discovery and optimization has driven the rapid technological advancements that have been observed in our lifetimes. For this advancement to continue, solid-state chemists must continue to develop new materials. Where do these new materials come from? In this review, we discuss the approaches used by the zur Loye group to discover the next “First Material”, a new material exhibiting a desired or not previously observed property that can be optimized for use in the technologies of tomorrow. Specifically, we discuss several crystal growth techniques that we have used with great success to synthesize new materials: the flux growth method, the hydroflux method, and the mild-hydrothermal method. materials, the ever-shrinking cell phone due to improved INTRODUCTION microwave dielectric materials, the enhancement in lithium battery storage capacity due to new intercalation materials, and the improved capacitor due to new ferroelectric materials are all In our complex lives of the 21st Century we rely on technology and excellent examples of materials that were developed only recently. technological devices that work because they contain advanced We should not for one second believe, however, that these materials that exhibit specific properties to perform specific materials were discovered and used without further optimization, functions. -
2. Petrology and Mineralogy
2. Petrology and Mineralogy In the period from 1999 to 2002, many studies on petrology and mineralogy have been made by Japanese earth scientists as well as the previous period. Significant progress has been made at the Japanese-USA cooperative studies on Hawaiian volcanoes (Naka et al., 2000; see section VII of this report), including deep-sea survey with the submersible "Shinkai 6500", the world's most advanced deep-sea probe. Major part of the outcome was published as a monograph (Takahashi, E. et al., 2002), including petrological and geochemical studies on products collected by the deep-sea survey (Kaneoka et al., 2002; Sherman et al., 2002; Shinozaki et al., 2002; Tanaka et al., 2002) and melting experiments on basalt+peridotite (Takahashi, E. and Nakajima, 2002). Other studies on the Hawaii project were appeared as individual papers (e.g., Lipman et al., 2000). Research on Unzen volcano also progressed significantly after its eruption of 1990-1995 (Chen, C. H. et al., 1999; Kusakabe et al., 1999; Nakada and Motomura, 1999; Sato et al., 1999; Tateyama et al., 2002; Watanabe, Ko. et al., 1999). At the volcano, international scientific drilling project (Unzen volcano Scientific Drilling Project) is going on (Sakuma and Nakada, 2002; Sakuma and Saito, 2000; Uto et al., 2000; see section VII of this report) and many publications will be appeared in the next period. Research on subduction-zone magmatism around Japan was made energetically. As for Northeast Japan, spatial distribution of volcanoes was noticed (Umeda et al., 1999), and a new concept of "hot fingers" in the mantle wedge was proposed (Tamura, Y. -
Stratigraphy, Structure, and Petrology of the Mt. Cube Area, New Hampshire by Jarvis B
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA STRATIGRAPHY, STRUCTURE, AND PETROLOGY OF THE MT. CUBE AREA, NEW HAMPSHIRE BY JARVIS B. HADLEY CONTENTS Page Abstract.................................................................................................................................. 115 Introduction.......................................................................................................................... 115 Acknowledgments................................................................................................................. 117 Stratified rocks....................................................................................................................... 117 General statement........................................................................................................ 117 Orfordville formation................................................................................................... 119 General statement................................................................................................ 119 Post Pond volcanic member............................................................................... 119 Black schist............................................................................................................ 121 Hardy Hill qu&rtzite............................................................................................ 122 Sunday Mountain volcanic member................................................................. 123 Low-grade rocks of the Orfordville -
Magma Genesis, Plate Tectonics, and Chemical Differentiation of the Earth
REVIEWS OF GEOPHYSICS, VOL. 26, NO. 3, PAGES 370-404, AUGUST 1988 Magma Genesis, Plate Tectonics, and Chemical Differentiation of the Earth PETER J. WYLLIE Division of Geolo•7icaland Planetary Sciences,California Institute of Technolo•Ty,Pasadena Magma genesis,migration, and eruption have played prominent roles in the chemical differentiation of the Earth. Plate tectonics has provided the framework of tectonic environments for different suites of igneousrocks and the dynamic mechanismsfor moving massesof rock into melting regions.Petrology is rooted in geophysics.Petrological and geophysicalprocesses are calibrated by the phase equilibria of the materials. The geochemistry of basalts and mantle xenoliths demonstrates that the mantle is hetero- geneous.The geochemical reservoirs are related to mantle convection, with interpretation of a mantle layered or stratified or peppered with blobs. Seismic tomography is beginning to reveal the density distribution of the mantle in three dimensions,and together with fluid mechanical models and interpreta- tion of the geoid, closer limits are being placed on mantle convection. Petrological cross sectionscon- structed for various tectonic environments by transferring phase boundaries for source rocks onto assumedthermal structuresprovide physical frameworks for consideration of magmatic and metasoma- tic events,with examplesbeing given for basalts,andesites, and granites at ocean-continentconvergent plate boundaries, basalts and nephelinitesfrom a thermal plume beneath Hawaii, kimberlites in cratons, -
Mineralogy & Petrology
11/20/2006 COLLEGE OF SCIENCE AND HEALTH ENVIRONMENTAL SCIENCE COURSE OUTLINE 1. TITLE OF COURSE AND COURSE NUMBER: Mineralogy & Petrology ENV 270, 3 credits 2. DESCRIPTION OF THE COURSE: This course provides an introduction to the study of Earth Materials – rocks and minerals – their description, classification and origin. 3. COURSE PREREQUISITES: ENV 115 4. COURSE OBJECTIVES: To provide students with an introduction to the identification, classification and interpretation of the occurrence of rock-forming minerals and rocks. To provide the essentials of crystallographic theory and practice sufficient to understand the underlying structure of minerals; and, to relate the occurrence of various rock types to current plate tectonic theory. 5. STUDENT LEARNING OUTCOMES: Students should be able to: 1. Effectively express themselves in written and oral form on topics dealing with Earth materials. 2. Demonstrate the ability to think critically about Earth material issues through either writing or discussion. 3. Locate and use information on Earth material topics from a variety of sources, including peer-reviewed literature and electronic sources. 4. Demonstrate the ability to integrate knowledge of Earth materials and their significance in a coherent and meaningful manner. 5. Work effectively with others in gathering research information. 6. Be able to identify the major types of rock-forming minerals and rock under both field and laboratory conditions. 7. The basic principles of the identification of rocks and minerals in thin section – optical mineralogy. 8. Relate fundamental mineral properties to their underlying crystallographic structure. 9. Be able to place the petrology of rock within their fundamental plate tectonic context. 6. -
Crystallization Processes and Solubility of Columbite-(Mn), Tantalite-(Mn), Microlite, Pyrochlore, Wodginite and Titanowodginite in Highly Fluxed Haplogranitic Melts
Western University Scholarship@Western Scholarship@Western Electronic Thesis and Dissertation Repository 3-12-2018 10:30 AM Crystallization processes and solubility of columbite-(Mn), tantalite-(Mn), microlite, pyrochlore, wodginite and titanowodginite in highly fluxed haplogranitic melts Alysha G. McNeil The University of Western Ontario Supervisor Linnen, Robert L. The University of Western Ontario Co-Supervisor Flemming, Roberta L. The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Doctor of Philosophy © Alysha G. McNeil 2018 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Earth Sciences Commons Recommended Citation McNeil, Alysha G., "Crystallization processes and solubility of columbite-(Mn), tantalite-(Mn), microlite, pyrochlore, wodginite and titanowodginite in highly fluxed haplogranitic melts" (2018). Electronic Thesis and Dissertation Repository. 5261. https://ir.lib.uwo.ca/etd/5261 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Abstract Niobium and tantalum are critical metals that are necessary for many modern technologies such as smartphones, computers, cars, etc. Ore minerals of niobium and tantalum are typically associated with pegmatites and include columbite, tantalite, wodginite, titanowodginite, microlite and pyrochlore. Solubility and crystallization mechanisms of columbite-(Mn) and tantalite-(Mn) have been extensively studied in haplogranitic melts, with little research into other ore minerals. A new method of synthesis has been developed enabling synthesis of columbite-(Mn), tantalite-(Mn), hafnon, zircon, and titanowodginite for use in experiments at temperatures ≤ 850 °C and 200 MPa, conditions attainable by cold seal pressure vessels. -
Reviews in Economic Geology, Vol. 20
REVIEWS IN ECONOMIC GEOLOGY Volume 20 DIVERSITY OF CARLIN-STYLE GOLD DEPOSITS Editor John L. Muntean Ralph J. Roberts Center for Research in Economic Geology Nevada Bureau of Mines and Geology University of Nevada Reno SOCIETY OF ECONOMIC GEOLOGISTS, INC. Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/4617793/edocrev20fm.pdf by guest on 30 September 2021 REVIEWS IN ECONOMIC GEOLOGY Published by the Society of Economic Geologists, Inc. 7811 Shaffer Parkway Littleton, CO 80127, USA Website: segweb.org E-mail: [email protected] Printed by: robinprint 9457 S. University Blvd., #807 Highlands Ranch, CO 80126-4976 Email: [email protected] ISSN 0741–0123 (Print) 2374–443X (PDF) ISBN 978–1–629492–22–3 (Print) 978–1–629495–78–1 (PDF) Reviews in Economic Geology is a series publication of the Society of Economic Geolo- gists designed to accompany the Society’s Short Course series. Like the Short Courses, each volume provides comprehensive updates on various applied and academic topics for practicing economic geologists and geochemists in exploration, development, research, and teaching. Volumes are produced in conjunction with each new Short Course, first serving as a textbook for that course and subsequently made available to SEG members and others at a modest cost. On the cover: Map showing locations of Carlin-style gold deposits discussed in this volume: Great Basin, Nevada; Dian- Qian-Gui “Golden Triangle,” SW China; Nadaleen trend, Yukon, Canada; Bau district, Sarawak, Malaysia; Agdarreh and Zarshouran deposits, NW Iran; and Allchar deposit, Republic of Macedonia. Inset shows possible interrelationships between various sources of ore fluid and types of Carlin-style deposits, described in the introduction by Muntean in this volume. -
Compilation of Crystal Growers and Crystal Growth Projects Research Materials Information Center
' iW it( 1 ' ; cfrv-'V-'T-'X;^ » I V' 1l1 II V/ f ,! T-'* «( V'^/ l "3 ' lyJ I »t ; I« H1 V't fl"j I» I r^fS' ^SllMS^W'/r V '^Wl/ '/-D I'ril £! ^ - ' lU.S„AT(yMIC-ENERGY COMMISSION , : * W ! . 1 I i ! / " n \ V •i" "4! ) U vl'i < > •^ni,' 4 Uo I 1 \ , J* > ' . , ' ^ * >- ' y. V * / 1 \ ' ' i S •>« \ % 3"*V A, 'M . •. X * ^ «W \ 4 N / . I < - Vl * b >, 4 f » ' ->" ' , \ .. _../.. ~... / -" ' - • «.'_ " . Ife .. -' < p / Jd <2- ORNL-RMIC-12 THIS DOCUMENT CONFIRMED AS UNCLASSIFIED DIVISION OF CLASSIFICATION COMPILATION OF CRYSTAL GROWERS AND CRYSTAL GROWTH PROJECTS RESEARCH MATERIALS INFORMATION CENTER \i J>*\,skJ if Printed in the United States of America. Available from National Technical Information Service U.S. Department of Commerce 5285 Port Royal Road, Springfield, Virginia 22t51 Price: Printed Copy $3.00; Microfiche $0.95 This report was prepared as an account of work sponsored by the United States Government. Neither the United States nor the United States Atomic Energy Commission, nor any of their employees, nor any of their contractors, subcontractors, or their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness or usefulness of any information, apparatus, product or process disclosed, or represents that its use would not infringe privately owned rights. ORNL-RMIC-12 UC-25 - Metals, Ceramics, and Materials Contract No. W-7405-eng-26 COMPILATION OF CRYSTAL GROWERS AND CRYSTAL GROWTH PROJECTS T. F. Connolly Research Materials Information Center Solid State Division NOTICE This report was prepared as an account of work sponsored by the Unitsd States Government.