Week of May 4 – May 10
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Origin, Texture, and Classification of Metamorphic Rocks - Teklewold Ayalew
GEOLOGY – Vol. II - Origin, Texture, and Classification of Metamorphic Rocks - Teklewold Ayalew ORIGIN, TEXTURE, AND CLASSIFICATION OF METAMORPHIC ROCKS Teklewold Ayalew Addis Ababa University, Ethiopia Keywords: aluminosilicates, assemblage, fabric, foliation, gneissose banding, index mineral, isograd, lineation, lithosphere, metamorphic facies, metasomatism, orogenic belt, schistosity Contents 1. Introduction 2. Occurrence 2.1. Orogenic Metamorphism 2.2. Contact Metamorphism 2.3. Ocean Floor Metamorphism 3. Classification 4. Minerals of Metamorphic Rocks 5. Metamorphic Facies 5.1. Facies of Very Low Grade 5.2. Greenschist Facies 5.3. Amphibolite Facies 5.4. Granulite Facies 5.5. Hornblende Hornfels Facies 5.6. Pyroxene Hornfels Facies 5.7. Blueschist Facies 5.8. Eclogite Facies 6. Tectonic Setting of Metamorphic Facies 7. Textures 7.1. Layering, Banding, and Fabric Development 8. Kinetics 8.1. Diffusion 8.2. Nucleation 8.3. Crystal Growth AcknowledgmentUNESCO – EOLSS Glossary Bibliography Biographical SketchSAMPLE CHAPTERS Summary Metamorphic rocks are igneous, sedimentary, or other metamorphic rocks whose texture and composition has been changed by metamorphism. Metamorphism occurs as a response to changes in the physical or chemical environment of any pre-existing rock, such as variations in pressure or temperature, strain, or the infiltration of fluids. It involves recrystallization of existing minerals into new grains and/or the appearance of new mineral phases and breakdown of others. Metamorphic processes take place ©Encyclopedia of Life Support Systems (EOLSS) GEOLOGY – Vol. II - Origin, Texture, and Classification of Metamorphic Rocks - Teklewold Ayalew essentially in the solid state. The rock mass does not normally disaggregate and lose coherence entirely; however small amounts of fluids are frequently present and may play an important catalytic role. -
Facies and Mafic
Metamorphic Facies and Metamorphosed Mafic Rocks l V.M. Goldschmidt (1911, 1912a), contact Metamorphic Facies and metamorphosed pelitic, calcareous, and Metamorphosed Mafic Rocks psammitic hornfelses in the Oslo region l Relatively simple mineral assemblages Reading: Winter Chapter 25. (< 6 major minerals) in the inner zones of the aureoles around granitoid intrusives l Equilibrium mineral assemblage related to Xbulk Metamorphic Facies Metamorphic Facies l Pentii Eskola (1914, 1915) Orijärvi, S. l Certain mineral pairs (e.g. anorthite + hypersthene) Finland were consistently present in rocks of appropriate l Rocks with K-feldspar + cordierite at Oslo composition, whereas the compositionally contained the compositionally equivalent pair equivalent pair (diopside + andalusite) was not biotite + muscovite at Orijärvi l If two alternative assemblages are X-equivalent, l Eskola: difference must reflect differing we must be able to relate them by a reaction physical conditions l In this case the reaction is simple: l Finnish rocks (more hydrous and lower MgSiO3 + CaAl2Si2O8 = CaMgSi2O6 + Al2SiO5 volume assemblage) equilibrated at lower En An Di Als temperatures and higher pressures than the Norwegian ones Metamorphic Facies Metamorphic Facies Oslo: Ksp + Cord l Eskola (1915) developed the concept of Orijärvi: Bi + Mu metamorphic facies: Reaction: “In any rock or metamorphic formation which has 2 KMg3AlSi 3O10(OH)2 + 6 KAl2AlSi 3O10(OH)2 + 15 SiO2 arrived at a chemical equilibrium through Bt Ms Qtz metamorphism at constant temperature and = -
Rocks and Geology: General Information
Rocks and Geology: General Information Rocks are the foundation of the earth. Rock provides the firmament beneath our oceans and seas and it covers 28% of the earth's surface that we all call home. When we travel any distance in any given direction, it is impossible not to see the tremendous variety in color, texture, and shape of the rocks around us. Rocks are composed of one or more minerals. Limestone, for example, is composed primarily of the mineral calcite. Granite can be made up of the minerals quartz, orthoclase and plagioclase feldspars, hornblende, and biotite mica. Rocks are classified by their mineral composition as well as the environment in which they were formed. There are three major classifications of rocks: igneous, sedimentary and metamorphic. A question: Which kind of rock came first? Think about it....... The following sections describe the conditions and processes that create the landscape we admire and live on here on "terra firma." IGNEOUS ROCKS The millions of tons of molten rock that poured out of the volcano Paracutin in Mexico, and from the eruption of Mount St. Helens in Washington State illustrate one of the methods of igneous rock formation. Igneous (from fire) rocks are formed when bodies of hot liquid rock called magma located beneath the earth's crust, find their way upward through the crust by way of fissures or faults. If the magma reaches the earth's surface, it forms extrusive igneous rocks or volcanic rocks. If the magma cools before it reaches the surface, it forms bodies of rock called intrusive igneous rocks or plutonic rocks. -
Towards a Unified Nomenclature in Metamorphic Petrology
8. Amphibolite and Granulite Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: Web version 01.02.07 1José Coutinho, 2Hans Kräutner, 3Francesco Sassi, 4Rolf Schmid and 5Sisir Sen. 1 J. Coutinho, University of São Paulo, São Paulo, Brazil 2 L M University, Munich, Germany 3 F. Sassi, Department of Mineralogy and Petrography, University of Padova, Italy 4 R. Schmid, ETH-Centre, Zürich, Switzerland 5 S. Sen, Indian Institute of Technology, Kharagpur, India Introduction This paper summarises the results of the discussions by the SCMR, and the response to circulars distributed by the SCMR, which demonstrated the highly variable usage of the terms granulite and amphibolite. It presents those definitions which currently seem to be the most appropriate ones. Some notes are included in order to explain the reasoning behind the suggested definitions. In considering the definitions it is important to remember that some of them are a compromise of highly different, even conflicting, opinions and traditions. The names amphibolite and granulite have been used in geological literature for nearly 200 years: amphibolite since Brongniart (1813), granulite since Weiss (1803). Although Brongniart described amphibolite as a rock composed of amphibole and plagioclase, in those early days the meaning of the term was variable. Only later (e.g. Rosenbusch, 1898) was it fixed as metamorphic rock consisting of hornblende and plagioclase, and of medium to high metamorphic grade. In contrast, the use of the name granulite was highly variable, a position which was further complicated by the introduction of the facies principle (Eskola, 1920, 1952) when the name granulite was proposed for all rocks of the granulite facies. -
Oregon Geologic Digital Compilation Rules for Lithology Merge Information Entry
State of Oregon Department of Geology and Mineral Industries Vicki S. McConnell, State Geologist OREGON GEOLOGIC DIGITAL COMPILATION RULES FOR LITHOLOGY MERGE INFORMATION ENTRY G E O L O G Y F A N O D T N M I E N M E T R R A A L P I E N D D U N S O T G R E I R E S O 1937 2006 Revisions: Feburary 2, 2005 January 1, 2006 NOTICE The Oregon Department of Geology and Mineral Industries is publishing this paper because the infor- mation furthers the mission of the Department. To facilitate timely distribution of the information, this report is published as received from the authors and has not been edited to our usual standards. Oregon Department of Geology and Mineral Industries Oregon Geologic Digital Compilation Published in conformance with ORS 516.030 For copies of this publication or other information about Oregon’s geology and natural resources, contact: Nature of the Northwest Information Center 800 NE Oregon Street #5 Portland, Oregon 97232 (971) 673-1555 http://www.naturenw.org Oregon Department of Geology and Mineral Industries - Oregon Geologic Digital Compilation i RULES FOR LITHOLOGY MERGE INFORMATION ENTRY The lithology merge unit contains 5 parts, separated by periods: Major characteristic.Lithology.Layering.Crystals/Grains.Engineering Lithology Merge Unit label (Lith_Mrg_U field in GIS polygon file): major_characteristic.LITHOLOGY.Layering.Crystals/Grains.Engineering major characteristic - lower case, places the unit into a general category .LITHOLOGY - in upper case, generally the compositional/common chemical lithologic name(s) -
A Systematic Nomenclature for Metamorphic Rocks
A systematic nomenclature for metamorphic rocks: 1. HOW TO NAME A METAMORPHIC ROCK Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: Web version 1/4/04. Rolf Schmid1, Douglas Fettes2, Ben Harte3, Eleutheria Davis4, Jacqueline Desmons5, Hans- Joachim Meyer-Marsilius† and Jaakko Siivola6 1 Institut für Mineralogie und Petrographie, ETH-Centre, CH-8092, Zürich, Switzerland, [email protected] 2 British Geological Survey, Murchison House, West Mains Road, Edinburgh, United Kingdom, [email protected] 3 Grant Institute of Geology, Edinburgh, United Kingdom, [email protected] 4 Patission 339A, 11144 Athens, Greece 5 3, rue de Houdemont 54500, Vandoeuvre-lès-Nancy, France, [email protected] 6 Tasakalliontie 12c, 02760 Espoo, Finland ABSTRACT The usage of some common terms in metamorphic petrology has developed differently in different countries and a range of specialised rock names have been applied locally. The Subcommission on the Systematics of Metamorphic Rocks (SCMR) aims to provide systematic schemes for terminology and rock definitions that are widely acceptable and suitable for international use. This first paper explains the basic classification scheme for common metamorphic rocks proposed by the SCMR, and lays out the general principles which were used by the SCMR when defining terms for metamorphic rocks, their features, conditions of formation and processes. Subsequent papers discuss and present more detailed terminology for particular metamorphic rock groups and processes. The SCMR recognises the very wide usage of some rock names (for example, amphibolite, marble, hornfels) and the existence of many name sets related to specific types of metamorphism (for example, high P/T rocks, migmatites, impactites). -
Metamorphic Rocks
Metamorphic Rocks Geology 200 Geology for Environmental Scientists Regionally metamorphosed rocks shot through with migmatite dikes. Black Canyon of the Gunnison, Colorado Metamorphic rocks from Greenland, 3.8 Ga (billion years old) Major Concepts • Metamorphic rocks can be formed from any rock type: igneous, sedimentary, or existing metamorphic rocks. • Involves recrystallization in the solid state, often with little change in overall chemical composition. • Driving forces are changes in temperature, pressure, and pore fluids. • New minerals and new textures are formed. Major Concepts • During metamorphism platy minerals grow in the direction of least stress producing foliation. • Rocks with only one, non-platy, mineral produce nonfoliated rocks such as quartzite or marble. • Two types of metamorphism: contact and regional. Metamorphism of a Granite to a Gneiss Asbestos, a metamorphic amphibole mineral. The fibrous crystals grow parallel to least stress. Two major types of metamorphism -- contact and regional Major Concepts • Foliated rocks - slate, phyllite, schist, gneiss, mylonite • Non-foliated rocks - quartzite, marble, hornfels, greenstone, granulite • Mineral zones are used to recognize metamorphic facies produced by systematic pressure and temperature changes. Origin of Metamorphic Rocks • Below 200oC rocks remain unchanged. • As temperature rises, crystal lattices are broken down and reformed with different combinations of atoms. New minerals are formed. • The mineral composition of a rock provides a key to the temperature of formation (Fig. 6.5) Fig. 6.5. Different minerals of the same composition, Al2SiO5, are stable at different temperatures and pressures. Where does the heat come from? • Hot magma ranges from 700-12000C. Causes contact metamorphism. • Deep burial - temperature increases 15-300C for every kilometer of depth in the crust. -
Stratigraphy of Ontario Ridge Metasediments
Pseudo-stratigraphic Column of Ontario Ridge Metasediments Member 10: Upper portion leucocratic migmatite with minor melanocratic gneiss and locally containing small pods of hornblende rock derived from marble; melanocratic gneiss in lower portion; large swath of marble in lower portion with basal calc-silicate and calc-silicate east of Bighorn Peak, sparse quartzite outcrops. Also includes quartzite layer near Shortcut Ridge with several feet of biotite-hornblende-quartz gneiss near center. *Migmatite: light gray, medium to ne-grained; vague irregular compositional layering, layers locally intrude one another; ptygmatically folded; thin irregular aplite bodies common; average composition about 55% feldspar, 35% quartz and 10% hornblende; biotite locally present; scattered euhedra of sphene usually visible in hand specimen. *Melanocratic gneiss: conspicuously banded with dark gray layers a fraction of an inch to several inches thick alternating with whitish gray layers mostly less 10 than two inches thick; layers irregularly to semiregularly folded with wavelengths of a few inches; fold axes subparallel; dark layers ne-grained, foliated, compositionally variable but typically about 60% hornblende and/or biotite, 30% plagioclase and 10% quartz; light layers ne- to medium-grained; aplitic in appearance, lenticular with irregular shapes, composed of quartz and feldspar. *Quartzite: light gray, granoblastic, ne- to medium-grained; very thin poorly-dened bedding; tightly folded in most outcrops with fold amplitudes of a few inches to a few feet, sheared folds locally simulate crossbedding; average quartz content about 80%, biotite most common accessory. 210 meter thickness Member 9: Gneisses and migmatites dominant; migmatite extensively developed along south side of Icehouse Canyon; roughly 50 feet of dolomite marble and minor calc-silicate rocks 250 feet below top of member; minor marble and calc-silicate rocks interbedded near base; graphite-rich schists locally present. -
Metamorphic Rocks -- Rocks That Change by Cindy Grigg
Metamorphic Rocks -- Rocks that Change By Cindy Grigg 1 Rocks can be put into three main groups. They are grouped by how the rocks formed. Metamorphic (met-uh-MOR-fic) rocks are changed by the heat and pressure inside Earth. "Metamorphic" comes from a Greek word that means "change of form." Metamorphic rocks can be formed from other metamorphic rocks. They can form from sedimentary and igneous rocks, too. 2 The temperature deep inside the Earth is much hotter than temperatures near or on the surface. The weight of tons of land and rocks on top presses down on the rocks underneath. This pressure, along with heat, causes the rocks inside the Earth to go through a physical or chemical change. Movement of Earth's plates causes pressure on rocky material under the surface, resulting in folding. Water can dissolve and redeposit minerals. This can also cause a change in rocks. Minerals react with each other at high heat. Atoms rearrange, and new minerals are created from old ones. Grains in rocks are pressed and made more compact. Rocks morph into other kinds of rocks. 3 Some metamorphic rocks are slate, schist, gneiss, marble, and quartzite. Sandstone is a sedimentary rock. It is made of grains of sand pressed together. Sandstone is fairly soft. It crumbles easily. When sandstone changes into the metamorphic rock quartzite, is becomes one of the hardest rocks. 4 The sedimentary rock shale changes into slate. The mineral grains in shale change directions because of the heat and pressure. Slate, a metamorphic rock, can be changed by continued heat and pressure into a rock called schist. -
Glossary of Geological Terms
GLOSSARY OF GEOLOGICAL TERMS These terms relate to prospecting and exploration, to the regional geology of Newfoundland and Labrador, and to some of the geological environments and mineral occurrences preserved in the province. Some common rocks, textures and structural terms are also defined. You may come across some of these terms when reading company assessment files, government reports or papers from journals. Underlined words in definitions are explained elsewhere in the glossary. New material will be added as needed - check back often. - A - A-HORIZON SOIL: the uppermost layer of soil also referred to as topsoil. This is the layer of mineral soil with the most organic matter accumulation and soil life. This layer is not usually selected in soil surveys. ADIT: an opening that is driven horizontally (into the side of a mountain or hill) to access a mineral deposit. AIRBORNE SURVEY: a geophysical survey done from the air by systematically crossing an area or mineral property using aircraft outfitted with a variety of sensitive instruments designed to measure variations in the earth=s magnetic, gravitational, electro-magnetic fields, and/or the radiation (Radiometric Surveys) emitted by rocks at or near the surface. These surveys detect anomalies. AIRBORNE MAGNETIC (or AEROMAG) SURVEYS: regional or local magnetic surveys that measures deviations in the earth=s magnetic field and carried out by flying a magnetometer along flight lines on a pre-determined grid pattern. The lower the aircraft and the closer the flight lines, the more sensitive is the survey and the more detail in the resultant maps. Aeromag maps produced from these surveys are important exploration tools and have played a major role in many major discoveries (e.g., the Olympic Dam deposit in Australia). -
Some Notes on the Geology of King Island
Tasmanian Geological Survey Record 2007/02 SSoommee nnootteess oonn tthhee ggeeoollooggyy ooff KKiinngg IIssllaanndd Department of In frastructure, Energy and Resources Mineral Resources Tasmania Tasmanian Geological Survey Record 2007/02 Some notes on the geology of King Island by C . R. Calver Department of Infrastructure, EnergTasmaniany and R Geologicalesourc eSurveys Record 2007/02 1 Mineral Resources Tasmania Mineral Resources Tasmania PO Box 56 Rosny Park Tasmania 7018 Phone: (03) 6233 8377 l Fax: (03) 6233 8338 Email: [email protected] l Internet: www.mrt.tas.gov.au 2 Tasmanian Geological Survey Record 2007/02 Contents Summary ………………………………………………………………………………… 3 Western King Island ……………………………………………………………………… 5 Surprise Bay Formation ………………………………………………………………… 5 Regional deformation and metamorphism………………………………………………… 5 Granitoid intrusion and local deformation………………………………………………… 6 Eastern King Island ……………………………………………………………………… 6 Naracoopa Formation …………………………………………………………………… 6 Grassy Group…………………………………………………………………………… 6 Base of the Ediacaran ……………………………………………………………………… 9 Devonian granites and contact metamorphism and metasomatism …………………………… 9 Scheelite deposits ………………………………………………………………………… 9 Tertiary–Quaternary ……………………………………………………………………… 12 Detailed location descriptions ……………………………………………………………… 13 Western King Island …………………………………………………………………… 13 Cape Wickham………………………………………………………………………… 13 Ettrick Beach ………………………………………………………………………… 14 Seal Rocks State Reserve ……………………………………………………………… 14 City of Melbourne Bay area ……………………………………………………………… -
Geological Archive of the Onset of Plate Tectonics
View metadata, citation and similar papers at core.ac.uk brought to you by CORE Geological archive of the onsetprovided by espace@Curtin of plate tectonics rsta.royalsocietypublishing.org Peter A. Cawood1,2, Chris J. Hawkesworth2,3, Sergei A. Pisarevsky4, Bruno Dhuime3,5, 1 1 Research Fabio A. Capitanio andOliverNebel 1 Cite this article: Cawood PA, Hawkesworth School of Earth, Atmosphere and Environment, Monash University, CJ, Pisarevsky SA, Dhuime B, Capitanio FA, Melbourne, VIC 3800, Australia 2 Nebel O. 2018 Geological archive of the onset Department of Earth Sciences, University of St Andrews, of plate tectonics. Phil.Trans.R.Soc.A376: St Andrews, Fife KY16 9AL, UK 20170405. 3School of Earth Sciences, University of Bristol, Wills Memorial http://dx.doi.org/10.1098/rsta.2017.0405 Building, Queens Road, Bristol BS8 1RJ, UK 4ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and Accepted:21June2018 Earth Dynamics Research Group, The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin One contribution of 14 to a discussion meeting University, GPO Box U1987, Perth, WA 6845, Australia issue‘Earthdynamicsandthedevelopmentof 5CNRS-UMR 5243, Géosciences Montpellier, Université de plate tectonics’. Montpellier, Montpellier, France Subject Areas: PAC, 0000-0003-1200-3826;BD,0000-0002-4146-4739; plate tectonics, geochemistry, geology ON, 0000-0002-5068-7117 Keywords: Plate tectonics, involving a globally linked system of lateral motion of rigid surface plates, is a plate tectonics, Archaean, palaeomagnetics, characteristic feature of our planet, but estimates lithosphere, early Earth of how long it has been the modus operandi of lithospheric formation and interactions range from Author for correspondence: the Hadean to the Neoproterozoic.