Petrology of the Metamorphic Rocks

Total Page:16

File Type:pdf, Size:1020Kb

Petrology of the Metamorphic Rocks Petrology of the metamorphic rocks Second Edition Roger Mason London UNWIN HYMAN Boston Sydney Wellington © R. Mason, 1990 This book is copyright under the Berne Convention. No reproduction without permission. All rights reserved. Published by the Academic Division of Unwin Hyman Ltd 15/17 Broadwick Street, London WIV IFP, UK Unwin Hyman Inc. 955 Massachusetts Avenue, Cambridge, MA 02139, USA Allen & Unwin (Australia) Ltd 8 Napier Street, North Sydney, NSW 2060, Australia Allen & Unwin (New Zealand) Ltd in association with the Port Nicholson Press Ltd Compusales Building, 75 Ghuznee Street, Wellington I, New Zealand First published in 1990 British Library Cataioguing in Publication Data Mason, Roger 1941- Petrology of the metamorphic rocks. - 2nd ed. I. Metamorphic rocks. Petrology I. Title 552.4 ISBN 978-0-04-552028-2 ISBN 978-94-010-9603-4 (eBook) DOI 10.1007/978-94-010-9603-4 Library of Congress Cataioging-in-Publication Data Mason, Roger, 1941- Petrology of the metamorphic rocks/Roger Mason. - 2nd ed. p. cm. Includes bibliographical references. 1. Rocks, Metamorphic. I. Title. QE475.A2M394 1990 552·.~c20 90-35106 CIP Typeset in 10 on 12 point Times by Computape (Pickering) Ltd, North Yorkshire Preface There has been a great advance in the understanding of processes of meta­ morphism and of metamorphic rocks since the last edition of this book appeared. Methods for determining temperatures and pressures have become almost routine, and there is a wide appreciation that there is not a single temperature and pressure of metamorphism, but that rocks may preserve, in their minerals, chemistry and textures, traces of their history of burial, heating, deformation and permeation by fluids. However, this excit­ ing new knowledge is still often difficult for non-specialists to understand, and this book, like the first edition, aims at enlightenment. I have concen­ trated on the interpretation of the plate tectonic settings of metamorphism, rather than following a geochemical approach. Although there is an impress­ ive degree of agreement between the two, I believe that attempting to discover the tectonic conditions accompanying rock recrystallization will more readily arouse the interest of the beginner. I have used a series of case histories, as in the first edition, drawing on my own direct experience as far as possible. This m~ns that some subjects are treated in more detail than others, and many important topics are barely mentioned at all. It also means that general concepts appear in a rather haphazard order in the text. To help my readers, I have provided a glossary of definitions of terms used in the book, which are indicated in bold type in the text. I discuss thermotectonic models, based on very simple 2-dimensio­ nal analyses, in describing the metamorphic history of many of my examples. Although many problems remain to be solved in this approach (and I do not claim that my models are sufficiently rigorous to be contributions to research discussion), its success in accounting for the shape of many P-T-t paths has convinced me that it is a useful framework to use in learning about meta­ morphisrri. I hope I have provided my readers with an interesting and sound basis for further exploration of this fascinating branch of the Earth sciences. The present form of the book arose from a course of lectures and demonstrations given at Wuhan College of Geology (since renamed the China University of Geosciences) in the People's Republic of China in 1986. I thank President Zhao Pengda and Professor You Zhendong for inviting me to give the course, Mrs Han Yuqing who worked very hard as my inter­ preter, and the students of the class who suffered the culture shock of being introduced to western-style discussion in lectures! I have been encouraged to PREFACE emphasize the tectonic theme in a thorough and constructive review of my manuscript by Dr M. J. Le Bas. In addition to those I thanked for advice in my first edition, I would like to thank Dr L. Ashwal, Dr A. P. Boyle, Professor K. Burke, Dr K. W. Burton, Mr A. J. Griffiths, Dr W. L. Kirk, Dr J. D. A. Piper, Dr G. D. Price, Ms K. V. Wright, Dr J. W. Valley, and Dr C. Xenophontos. I thank Dr P. W. Edmondson for compiling the index. I also acknowledge with thanks receipt of a travel grant from the Central Research Fund of the University of London to visit classic metamorphic localities in the USA, and also a grant from the Royal Society of London to the Sulitjelma '83 Ophiolite Expedition. Contents Preface page v List of tables IX 1 Introduction 1 Definition 1 The processes of metamorphism 2 The three field categories of metamorphic rocks 6 Studying thin sections of metamorphic rocks 8 Laboratory study of metamorphic rocks 9 Why study metamorphic rocks? 16 2 Rock and mineral compositions, and their relationship 18 Classification of metamorphic rocks 18 Chemical compositions of metamorphic rocks 26 The Phase Rule 28 Recognition of equilibrium in metamorphic rocks 32 Composition - assemblage diagrams 37 Metamorphic textures 44 Metamorphic facies 49 Thermotectonic modelling 53 3 Metamorphism associated with igneous intrusions 57 The Skiddaw contact aureole, Cumbria, England 64 The Beinn an Dubhaich aureole, Isle of Skye, Scotland 75 Compositions of fluids in contact metamorphism 84 Thermal models of contact metamorphism 86 viii CONTENTS 4 Dynamic metamorphism 94 The Mutki granitic mylonite, Turkey 95 The Lochseiten Mylonite, Switzerland 103 Dynamic metamorphism in relation to depth 105 5 Metamorphism associated with lithospheric extension 107 Metamorphism at spreading oceanic ridges 107 Metamorphism in sedimentary basins 119 6 Metamorphism in subduction zones 129 7 Metamorphism in collision zones 138 Metamorphic evolution of pelitic rocks of Connemara, Ireland 144 The Sulitjelma copper-mining district, Norway and Sweden 149 8 Metamorphism in stable continental crust 169 Metamorphism in Dengfeng County, Henan Province, China 175 Pyroxene gneisses of northwestern Scotland 177 The Adirondack Mountains, New York State, USA 184 Heat flow and thermal gradients in continental crust 189 9 Metamorphic rocks of the mantle 191 10 Extraterrestrial metamorphism 199 Impact metamorphism 199 Shock metamorphism at the Nordlinger Ries crater, Germany 200 Metamorphism in Moon rocks 205 Appendix 208 Glossary 209 References 220 Index 225 List of tables Table 1.1 Pressure units used in petrology. page 6 Table 2.1 Scheme of classification of metamorphic rocks in the field. 25 Table 2.2 Calculation of ACF values for an analysed basic igneous rock. 40 Table 2.3 Calculation of AFM values for a pelitic rock. 42 Table 2.4 Names of metamorphic facies and typical mineral assem- blages of basic rocks and pelitic rocks in each. 52 Table 3.1 Analysis of Skiddaw slate compared with an analysis of andalusite. 69 Table 3.2 Tectonic and metamorphic history of the Skiddaw contact aureole. 75 Table 3.3 Reactions in the system CaO--MgO--Si02-C02 at a pressure of 101.3 kPa. 79 Table 3.4 Maximum contact temperatures T max computed for intru- sion of magma at temperature Tm into dry country rocks at temperature Te. 86 Table 4.1 Textural classification of mylonites. 102 For Marion .
Recommended publications
  • Editorial for Special Issue “Ore Genesis and Metamorphism: Geochemistry, Mineralogy, and Isotopes”
    minerals Editorial Editorial for Special Issue “Ore Genesis and Metamorphism: Geochemistry, Mineralogy, and Isotopes” Pavel A. Serov Geological Institute of the Kola Science Centre, Russian Academy of Sciences, 184209 Apatity, Russia; [email protected] Magmatism, ore genesis and metamorphism are commonly associated processes that define fundamental features of the Earth’s crustal evolution from the earliest Precambrian to Phanerozoic. Basically, the need and importance of studying the role of metamorphic processes in formation and transformation of deposits is of great value when discussing the origin of deposits confined to varied geological settings. In synthesis, the signatures imprinted by metamorphic episodes during the evolution largely indicate complicated and multistage patterns of ore-forming processes, as well as the polygenic nature of the mineralization generated by magmatic, postmagmatic, and metamorphic processes. Rapid industrialization and expanding demand for various types of mineral raw ma- terials require increasing rates of mining operations. The current Special Issue is dedicated to the latest achievements in geochemistry, mineralogy, and geochronology of ore and metamorphic complexes, their interrelation, and the potential for further prospecting. The issue contains six practical and theoretical studies that provide for a better understanding of the age and nature of metamorphic and metasomatic transformations, as well as their contribution to mineralization in various geological complexes. The first article, by Jiang et al. [1], reports results of the first mineralogical–geochemical Citation: Serov, P.A. Editorial for studies of gem-quality nephrite from the major Yinggelike deposit (Xinjiang, NW China). Special Issue “Ore Genesis and The authors used a set of advanced analytical techniques, that is, electron probe microanaly- Metamorphism: Geochemistry, sis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry Mineralogy, and Isotopes”.
    [Show full text]
  • Metamorphic Rocks (Lab )
    Figure 3.12 Igneous Rocks (Lab ) The RockSedimentary Cycle Rocks (Lab ) Metamorphic Rocks (Lab ) Areas of regional metamorphism Compressive Compressive Stress Stress Products of Regional Metamorphism Products of Contact Metamorphism Foliated texture forms Non-foliated texture forms during compression during static pressure Texture Minerals Other Diagnostic Metamorphic Protolith Features Rock Name Non-foliated calcite, dolomite cleavage faces of Marble Limestone calcite usually visible quartz quartz grains are Quartzite Quartz Sandstone intergrown Foliated clay looks like shale but Slate Shale breaks into layers muscovite, biotite very fine-grained, but Phyllite Shale has a sheen like satin muscovite, biotite, minerals are large Schist Shale may have garnet enough to see easily, muscovite and biotite grains are parallel to each other feldspar, biotite, has layers of different Gneiss Any protolith muscovite, quartz, minerals garnet amphibole layered black Amphibolite Basalt or Andesite amphibole grains Texture Minerals Other Diagnostic Metamorphic Protolith Features Rock Name Non-foliated calcite, dolomite cleavage faces of Marble Limestone calcite usually visible quartz quartz grains are Quartzite Quartz Sandstone intergrown Foliated clay looks like shale but Slate Shale breaks into layers muscovite, biotite very fine-grained, but Phyllite Shale has a sheen like satin muscovite, biotite, minerals are large Schist Shale may have garnet enough to see easily, muscovite and biotite grains are parallel to each other feldspar, biotite, has layers of different Gneiss Any protolith muscovite, quartz, minerals garnet amphibole layered black Amphibolite Basalt or Andesite amphibole grains Identification of Metamorphic Rocks 12 samples 7 are metamorphic 5 are igneous or sedimentary Protoliths and Geologic History For 2 of the metamorphic rocks: Match the metamorphic rock to its protolith (both from Part One) Write a short geologic history of the sample 1.
    [Show full text]
  • MSA PRESIDENTIAL ADDRESS Metamorphism and the Evolution of Subduction on Earth
    American Mineralogist, Volume 104, pages 1065–1082, 2019 MSA PRESIDENTIAL ADDRESS Metamorphism and the evolution of subduction on Earth MICHAEL BROWN1,* AND TIM JOHNSON2,3 1Laboratory for Crustal Petrology, Department of Geology, University of Maryland, College Park, Maryland 20742, U.S.A. Orcid 0000-0003-2187-616X 2School of Earth and Planetary Sciences, The Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, West Australia 6845, Australia. Orcid 0000-0001-8704-4396 3Center for Global Tectonics, State Key Laboratory for Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei Province, 430074, China ABSTRACT Subduction is a component of plate tectonics, which is widely accepted as having operated in a manner similar to the present-day back through the Phanerozoic Eon. However, whether Earth always had plate tectonics or, if not, when and how a globally linked network of narrow plate boundaries emerged are mat- ters of ongoing debate. Earth’s mantle may have been as much as 200–300 °C warmer in the Mesoarchean compared to the present day, which potentially required an alternative tectonic regime during part or all of the Archean Eon. Here we use a data set of the pressure (P), temperature (T), and age of metamorphic rocks from 564 localities that vary in age from the Paleoarchean to the Cenozoic to evaluate the petrogenesis and secular change of metamorphic rocks associated with subduction and collisional orogenesis at convergent plate boundaries. Based on the thermobaric ratio (T/P), metamorphic rocks are classified into three natural groups: high T/P type (T/P > 775 °C/GPa, mean T/P ~1105 °C/GPa), intermediate T/P type (T/P between 775 and 375 °C/GPa, mean T/P ~575 °C/GPa), and low T/P type (T/P < 375 °C/GPa, mean T/P ~255 °C/GPa).
    [Show full text]
  • The Metamorphosis of Metamorphic Petrology
    Downloaded from specialpapers.gsapubs.org on May 16, 2016 The Geological Society of America Special Paper 523 The metamorphosis of metamorphic petrology Frank S. Spear Department of Earth and Environmental Sciences, JRSC 1W19, Rensselaer Polytechnic Institute, 110 8th Street, Troy, New York 12180-3590, USA David R.M. Pattison Department of Geoscience, University of Calgary, 2500 University Drive NW, Calgary, Alberta T2N 1N4, Canada John T. Cheney Department of Geology, Amherst College, Amherst, Massachusetts 01002, USA ABSTRACT The past half-century has seen an explosion in the breadth and depth of studies of metamorphic terranes and of the processes that shaped them. These developments have come from a number of different disciplines and have culminated in an unprece- dented understanding of the phase equilibria of natural systems, the mechanisms and rates of metamorphic processes, the relationship between lithospheric tecton- ics and metamorphism, and the evolution of Earth’s crust and lithospheric mantle. Experimental petrologists have experienced a golden age of systematic investigations of metamorphic mineral stabilities and reactions. This work has provided the basis for the quantifi cation of the pressure-temperature (P-T) conditions associated with various metamorphic facies and eventually led to the development of internally con- sistent databases of thermodynamic data on nearly all important crustal minerals. In parallel, the development of the thermodynamic theory of multicomponent, multi- phase complex systems underpinned development of the major methods of quantita- tive phase equilibrium analysis and P-T estimation used today: geothermobarometry, petrogenetic grids, and, most recently, isochemical phase diagrams. New analytical capabilities, in particular, the development of the electron micro- probe, played an enabling role by providing the means of analyzing small volumes of materials in different textural settings in intact rock samples.
    [Show full text]
  • Metamorphic Rocks
    Metamorphism and metamorphic rocks GEOL115 Alexander Lusk Outline: • Metamorphic rocks – Defini>on and major types of metamorphism – Rock cycle • Metamorphic processes • Deformaon and development of a foliaon/ schistosity/cleavage • Progressive (prograde) metamorphic series • Environments of metamorphism • Metamorphic facies Metamorphic rocks If pre-exis>ng rocks (e.g. igneous, sedimentary, metamorphic) are buried within in the Earth, new minerals can grow in the solid rock through recrystallizaon and the rock can deform in response to tectonic forces. This rock may have started off as a sediment of mud or clay, which later become a sedimentary rock such as mudstone or shale … What minerals are present? Recall the rock cycle: Recall where different rock types form: Types of metamorphism Regional metamorphism: as rocks are buried deeper and deeper within the earth they are subject to increasingly higher pressures and temperatures, which result in recrystallization. The directed pressures (stresses) produce planar structures called foliation. Contact metamorphism: rocks within the crust that are intruded by magma are recrystallized by the magma’s high temperatures. These rocks are commonly not deformed (foliated). Processes involved: 1. Neomineralizaon – growth of new minerals replacing minerals that become unstable. 2. Grain growth – growth of new or exis>ng mineral grains. 3. Deformaon – creates a schistosity or foliaon defined by the orientaon of platy or elongate mineral grains. Neomineralizaon Porphyroblasts: Porphyroclasts: Grain growth:
    [Show full text]
  • Relative Dating of Rock Sequences Rocks Tell Their Stories All That Remains Is for Us to Observe and Infer Their History. 1
    Relative Dating of Rock Sequences Rocks Tell Their Stories All that remains is for us to observe and infer their history. Look at the 2 illustrations in this lesson which show several horizontally layered sedimentary rock layers, igneous intrusions and faults. They have been numbered and lettered for ease of reference. In this lesson we will tell the "story" of the rock sequences by observing certain characteristics: 1- The order in which the rock layers appear. 2- Erosional Surfaces 3- Unconformities If you need help with the submergence , emergence and unconformity issues, go to Submergence and Emergence of Rock Layers With Respect to Sea Level, look at the illustrations and read the captions. The Key: Be sure to look at the key before observing the series of illustrations. Notice that not only do symbols exist for sandstone, shale and conglomerate, but also for the loose sediments that will eventually lithify to become these rock types. Go On To Page 2 Let the Stories Begin! L. Immoor 2006 Geoteach.com 1 This is the "story" for Rock Sequence 1: 1- Submergence followed by Deposition and the Formation of layers 1 and 2 (the sandstone and limestone). 2- Emergence and Erosion of layer 2 (limestone). 3- Submergence followed by Deposition and the Formation of layer 3, (the shale) producing an unconformity with layer 2 (limestone). The unconformity is evidenced by the wavy, eroded top surface of a rock layer. 4- Igneous Intrusion A with resulting Contact Metamorphism of layers 1, 2 and 3 (the sandstone, limestone and shale). 5- Emergence and Erosion of layer 3 (shale) and Igneous Intrusion A.
    [Show full text]
  • 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).
    [Show full text]
  • Interpreting Rock Layers (Modified for Adeed)
    INTERPRETING ROCK LAYERS (MODIFIED FOR ADEED) Science Concept: Sedimentary rocks can be aged using the law of superposition. Unconformities can create exceptions to this law. Objectives: The student will: • explain how rocks are dated by relative position (superposition); • describe how unconformities can affect the position of rocks and their relative age; • make inferences about the relative age of rock layers; and • explain in writing how the law of superposition and knowledge of unconformities can help age rock layers. GLEs Addressed: Science [10] SD1.1 The student demonstrates an understanding of geochemical cycles by using a model to explain the processes (i.e., formation, sedimentation, erosion, reformation) of the rock cycle. [10] SA1.1 The student demonstrates an understanding of the processes of science by asking questions, predicting, observing, describing, measuring, classifying, making generalizations, analyzing data, developing models, inferring, and communicating. Writing [10] W4.2.2 The student writes for a variety of purposes and audiences by writing in a variety of nonfiction forms (e.g., letter, report, biography, autobiography, and/or essay) to inform, describe, or persuade. Vocabulary: conformity - A bedding surface separating younger from older strata, along which there is no evidence of subaerial or submarine erosion or of nondeposition, and along which there is no evidence of a significant hiatus. Unconformities (sequence boundaries) and flooding surfaces (parasequence boundaries) pass laterally into correlative conformities, or correlative surfaces igneous rock - rocks formed are hardened and cooled magma law of superposition - sedimentary layers are deposited in a time sequence, with the oldest on the bottom and the youngest on the top metamorphic rock - rocks formed from other rocks as a result of heat and pressure nonconformity - Nonconformity exists between sedimentary rocks and metamorphic or igneous rocks when the sedimentary rock lies above and was deposited on the pre-existing and eroded metamorphic or igneous rock.
    [Show full text]
  • Mixed-Layer Illite-Smectite in Pennsylvanian-Aged Paleosols: Assessing Sources of Illitization in the Illinois Basin
    minerals Article Mixed-Layer Illite-Smectite in Pennsylvanian-Aged Paleosols: Assessing Sources of Illitization in the Illinois Basin Julia A. McIntosh 1,* , Neil J. Tabor 1 and Nicholas A. Rosenau 2 1 Roy M. Huffington Department of Earth Sciences, Southern Methodist University, P.O. Box 750395, Dallas, TX 75275, USA; [email protected] 2 Ocean and Coastal Management Branch, Office of Wetlands Oceans and Watersheds, United States Environmental Protection Agency, Washington, DC 20004, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-214-768-2750 Abstract: Mixed-layer illite-smectite (I-S) from a new set of Pennsylvanian-aged Illinois Basin under- clays, identified as paleosols, are investigated to assess the impact of (1) regional diagenesis across the basin and (2) the extent to which ancient environments promoted illitization during episodes of soil formation. Interpretations from Reichweite Ordering and D◦ 2q metrics applied to X-ray diffraction patterns suggest that most I-S in Illinois Basin paleosols are likely the product of burial diagenetic processes and not ancient soil formation processes. Acid leaching from abundant coal units and hydrothermal brines are likely diagenetic mechanisms that may have impacted I-S in Pennsylvanian paleosols. These findings also suggest that shallowly buried basins (<3 km) such as the Illinois Basin may still promote clay mineral alteration through illitization pathways if maximum burial occurred in the deep past and remained within the diagenetic window for extended periods of time. More importantly, since many pedogenic clay minerals may have been geochemically reset during illitization, sources of diagenetic alteration in the Illinois Basin should be better understood if Citation: McIntosh, J.A.; Tabor, N.J.; Pennsylvanian paleosol minerals are to be utilized for paleoclimate reconstructions.
    [Show full text]
  • Module 22A Geological Laws GEOLOGIC LAWS
    Module 22A Geological Laws GEOLOGIC LAWS Geologic Laws ❑ Superposition ❑ Original Horizontality ❑ Original Continuity ❑ Uniformitarianism ❑ Cross-cutting Relationship ❑ Inclusions ❑ Faunal Succession Missing strata ❑ Unconformity ❑ Correlation Law of Superposition ❑ In an undisturbed rock sequence, the bottom layer of rock is older than the layer above it, or ❑ The younger strata at the top in an undisturbed sequence of sedimentary rocks. Law of Superposition Undisturbed strata Law of Superposition Disturbed strata Law of original horizontality ❑ Sedimentary rocks are laid down in horizontal or nearly horizontal layers, or ❑ Sedimentary strata are laid down nearly horizontally and are essentially paralel to the surface upon which they acummulate Law of Original Continuity ❑ The original continuity of water-laid sedimentary strata is terminated only by pincing out againts the basin of deposition, at the time of their deposition Law of Original Continuity Law of Original Continuity Law of Original Continuity NOTE: This law is considerable oversimplification. The last discoveries indicate that the termination is not necessarily at a basin border. Facies changes may terminated a strata. Uniformitarianism ❑ James Hutton (1726-1797) Scottish geologist developed the laws of geology ❑ Uniformitarianism is a cornerstone of geology ❑ Considered the Father of Modern Geology Uniformitarianism ❑ Uniformitarianism is based on the premise that: ➢ the physical and chemical laws of nature have remained the same through time ➢ present-day processes have operated throughout geologic time ➢ rates and intensities of geologic processes, and their results may have changed with time ❑ To interpret geologic events from evidence preserved in rocks ➢ we must first understand present-day processes and their results Uniformitarianism is a cornerstone of geology Uniformitarianism MODIFIED STATEMENT “The present is the key to the past" • The processes (plate tectonics, mountain building, erosion) we see today are believed to have been occurring since the Earth was formed.
    [Show full text]
  • Metamorphism and the Origin of Granitic Rocks Northgate District Colorado
    Metamorphism and the Origin of Granitic Rocks Northgate District Colorado GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-M Metamorphism and the Origin of Granitic Rocks Northgate District Colorado By T. A. STEVEN SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-M A discussion of the progressive metamorphism, granitixation, and local rheomorphism of a layered sequence of rocks, and of the later emplacement and deuteric alteration of an unrelated granitic stock UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Page Abstract_________________________________ 335 Pre-Cambrian geology—Continued Introduction-_______________________________________ 335 Dacite porphyry—____ ——— __ —— _____________ 364 Acknowledgments__ ___--_____-____-_____-______-_ 336 Intrusive quartz monzonite_-____--_-__-_--_-_-_. 365 Geologic setting._______ — _________________________ 336 Petrography ________—— —— _______________ 365 Pre-Cambrian geology—___________________________ 337 Main body of the stock____________— 366 Hornblende gneiss___-_________-_-_____-________ 338 Marginal dikes_________-____-__-__——— 366 Quartz monzonite gneiss_________________________ 342 Satellitic dikes___-___.__________ 367 Biotite-garnet gneiss___________________________ 345 Wall-rock alteration_________ _ __——_ 368 Pegmatite_________________________________
    [Show full text]
  • Precambrian Paleosols As Indicators of Paleoenvironments on the Early Earth
    PRECAMBRIAN PALEOSOLS AS INDICATORS OF PALEOENVIRONMENTS ON THE EARLY EARTH by Sherry Lynn Stafford B.S., University of Pittsburgh at Johnstown, 1995 M.S., University of Pittsburgh, 1999 Submitted to the Graduate Faculty of Arts and Sciences in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Pittsburgh 2007 UNIVERSITY OF PITTSBURGH FACULTY OF ARTS AND SCIENCES This dissertation was presented by Sherry Lynn Stafford It was defended on July 12, 2005 and approved by Hiroshi Ohmoto, Ph.D., Pennsylvania State University Charles E. Jones, Ph.D., University of Pittsburgh Edward G. Lidiak, Ph.D., University of Pittsburgh Brian W. Stewart, Ph.D., University of Pittsburgh Dissertation Advisor: Rosemary C. Capo, Ph.D., University of Pittsburgh ii Copyright © by Sherry Lynn Stafford 2007 iii PRECAMBRIAN PALEOSOLS AS INDICATORS OF PALEOENVIRONMENTS ON THE EARLY EARTH Sherry Lynn Stafford, Ph.D. University of Pittsburgh, 2007 Paleosols, or fossil soils, document past atmospheric composition, climate, and terrestrial landscapes and are key to understanding the composition and evolution of the Earth’s atmosphere and the environments in which life developed and evolved. Micromorphological, geochemical and isotopic studies of two Precambrian weathering profiles (Steep Rock, Canada and Hokkalampi, Finland) place constraints on the age of soil formation, document pedogenic processes and post-pedogenic alteration and metamorphism, and yield information about the terrestrial environment at a critical time in Earth history. The textures and geochemistry of the Early Proterozoic Hokkalampi paleosol and the Archean Steep Rock paleosol are consistent with in situ, subaerial weathering under varying soil redox conditions. The upper portion of both profiles have lost >40% of their iron relative to the parent material, similar to Phanerozoic vertisols, while retaining Fe3+/Fe2+ ratios >1.
    [Show full text]