THE INTERPRETATION OF IGNEOUS ROCKS

Size: px
Start display at page:

Download "THE INTERPRETATION OF IGNEOUS ROCKS"

Transcription

1 THE INTERPRETATION OF IGNEOUS ROCKS

2 TITLES OF RELATED INTEREST Boninites A. J. Crawford (ed.) Carbonatites K. Bell (ed.) Cathodoluminescence of geological materials D. J. Marshall Chemical fundamentals of geology R. Gill Crystal structures and cation sites of the rock-forming minerals J. R. Smyth & D. L. Bish The dark side of the Earth R. Muir Wood Deformation processes in minerals, ceramics and rocks D. J. Barber & P. G. Meredith (eds) Geology and mineral resources of West Africa J. B. Wright Igneous petrogenesis B. M. Wilson Image interpretation in geology S. Drury The inaccessible Earth G. C. Brown & A. E. Mussett Introduction to X-ray spectrometry K. L. Williams Komatiites N. Arndt & E. Nisbet (eds) Mathematics in geology J. Ferguson Metamorphism and metamorphic belts A. K. Miyashiro Perspectives on a dynamic Earth T. R. Paton Petrology of the igneous rocks F. Hatch et al. Petrology of the metamorphic rocks R. Mason Planetary landscapes R. Greeley A practical introduction to optical mineralogy C. D. Gribble & A. J. Hall Rheology of the Earth G. Ranalli Rutley's elements of mineralogy C. D. Gribble Simulating the Earth J. Holloway & B. Wood Statistical methods in geology R. F. Cheeney Volcanic successions R. Cas&J. V. Wright The young Earth E. G. Nisbet

3 THE INTERPRETATION OF IGNEOUS ROCKS K. G. Cox, 1. D. Bell and R. 1. Pankhurst [nnl Springer-Science+Business Media, B.v.

4 First edition 1979 Reprinted K.G. Cox, J.D.Bell and R.J. Pankhurst Originally published by Chapman & Hall in 1979 ISBN ISBN (ebook) DOI / Apart from any fair dealing for the purposes of research or private study, or criticism or review, as permitted under the UK Copyright Designs and Patents Act, 1988, this publication may not be reproduced, stored, or transmitted, in any form or by any means, without the prior permission in writing of the publishers, or in the case of reprographic reproduction only in accordance with the terms of the licences issued by the Copyright Licensing Agency in the UK, or in accordance with the terms of licences issued by the appropriate Reproduction Rights Organization outside the UK. Enquiries concerning reproduction outside the terms stated here should be sent to the publishers at the London address printed on this page. The publisher makes no representation, express or implied, with regard to the accuracy of the information contained in this book and cannot accept any legal responsibility or liability for any errors or omissions that may be made. A catalogue record for this book is available from the British Library Library of Congress Cataloging-in-Publication Data available

5 Now how Elephants should come to be buried in Churches, is a Question not easily answered... Robert Plot (1677)

6 Preface Our aim in writing this book is to try to show how igneous rocks can be persuaded to reveal some ofthe secrets of their origins. The data of igneous rocks consist of field relations, texture, mineralogy, and geochemistry. Additionally, experimental petrology tells us how igneous systems might be expected to behave. Working on this material we attempt to show how hypotheses concerning the origins and evolution of magmas are proposed and tested, and thus illuminate the interesting and fundamental problems of petrogenesis. The book assumes a modest knowledge of basic petrography, mineralogy, classification, and regional igneous geology. It has a role complementary to various established texts, several of which are descriptively good and give wide coverage and evaluation of petrogenetic ideas in various degrees of detail. Existing texts do not on the whole, however, deal with methodology, though this is one of the more important aspects of the subject. At first sight it may appear that the current work is a guidebook for the prospective research worker and thus has little relevance for the non-specialist student of geology. We hope this will prove to be far from the case. The methodological approach has an inherent interest because it can provide the reader with problems he can solve for himself, and as an almost incidental consequence he will acquire a satisfying understanding. Moreover, if the study of igneous rocks has any value at all for the non-specialist, it is at least as likely to lie in the scientific discipline of its methods as in any other aspect of the subject. This book is not built round any specific course. There is much in it that would be of benefit to and accessible to any undergraduate student of geology; but at the same time postgraduate students and even teachers of petrology may find it useful. In short, it is offered to petrologists of all ages. The authors are particularly grateful to R. W. Cleverly, P. J. Betton and D. Kiernan-Walker for their attempts to minimise the number of mistakes in the manuscript, and to Mrs P. Jackson for her excellent typing. Oxford 1978 K. G. Cox J. D. Bell R. J. Pankhurst

7 Contents Preface List of tables 1. Fractionation in igneous processes Introduction The concept of fractionation Classification of fractionation processes Open systems Summary page ix xiv Compositional variation in magmas Inter-element correlations Summary of progress Variation diagrams - introduction Triangular variation diagrams The liquid line-of-descent Phase diagrams - introduction Classification of systems Experimental method Representation of results The phase rule Construction of a phase diagram by the quenching method The reading of phase diagrams Binary diagrams Ternary systems - I Representation of composition Liquidus projections The solidus Primary phase fields Isothermal sections Equilibria involving two solids + liquid Equilibria involving three solids + liquid Equilibrium crystallisation and melting paths in ternary systems Fractional crystallisation paths Pseudo binary systems Some ternary systems of geological interest

8 xii Contents 5. Ternary systems with solid solutions page 120 Ternary solid solutions 130 The system diopside-albite-anorthite 131 The system nepheline-kalsilite-silica 133 Ternary feldspars The interpretation of two-element variation diagrams 145 Principles of the mixing calculation 146 Mixing calculations and the formulation of crystal fractionation hypotheses 147 Application to series of volcanic rocks 154 EXercises Petrographic aspects of volcanic rocks 176 Introduction 176 The phenocryst assemblage 176 Modal analysis of phenocrysts 181 Altered phenocrysts 181 Resorbed and mantled phenocrysts 183 Xenocrysts 187 Order of crystallisation 188 Quenching textures 189 Final products of solidification 192 Other groundmass textures Quaternary systems 197 Representation of composition 197 Sub-solidus joins 198 Liquidus diagrams 201 Crystallisation paths 202 Projection methods 205 The system forsterite-diopside-anorthite-silica Experimental work on natural basaltic and allied rocks 222 Introduction 222 Atmospheric pressure experiments 223 Computer simulation of crystallisation paths 238 High-pressure experiments on dry materials Water-bearing basic rock systems 258 Experiments on basaltic compositions 258 Experiments on synthetic peridotitic compositions 263 Experiments on natural peridotites 265 Phlogopite stability 267 The experiments of Nicholls and Ringwood (1973) Compositionally zoned magma bodies and their bearing on crystal settling 272 An ash-flow sheet from Aso caldera, south-western Japan 273 The Shamsan caldera sequence of Aden 276

9 Contents xiii A model for crystal settling in a non-convecting magma chamber Compensated crystal settling 12. Petrographic aspects of plutonic rocks Introduction Chilled margins Cumulates Sub-solidus textures Partial melting of plutonic rocks 13. The interpretation of data for plutonic rocks Volume of intrusions Time for emplacement of plutons Flow of magma Some thermal features of intrusions Convection in magmas Crystal settling Layered intrusions Some chemical features of layered intrusions 14. Trace elements in igneous processes Introduction Melting and crystallisation models More complex models Application of trace elements to petrogenesis 15. The use of isotopes in petrology Radiogenic isotope variations Strontium isotopes Neodymium isotopes Lead isotopes Stable isotope variations Further reading page Appendices 1. Nomenclature of igneous rocks Average major element compositions and CIPW norms of common igneous rock types Norm calculations 407 Calculation of the CIPW norm 408 Molecular norms Calculation of plotting parameters for O'Hara (1968) polybaric phase diagram Some representative mineral analyses 416 Answers to exercises 419 References 432 Index 446

10 List of Tables 1.1 States of matter in geological systems page Approximate equivalents of some K-rich and normal rock types Analyses of volcanic rocks from the Hanish-Zukur islands, Red Sea Total alkalis and silica contents of rocks termed trachyte and hawaiite in compilation of Carmichael et al. (1974) 40 2A Partial analyses of volcanic rocks Partial analyses of volcanic rocks Run data at 1000 C for the system A-B-C Analyses of compositions used in extract calculation Settling velocities of crystals in basic magma Analytical data for Exercise A Analytical data for Exercise Highest temperatures of crystallisation of major phases inkilauean lavas Calculation of plotting parameters for normative basalt system Rocks used to test normative basalt phase diagram 234 9A Chemical compositions and CIPW norms oftwo rocks investigated experimentally by Green and Ringwood (1967) Melting relations of AL and OT at various pressures Analyses of peridotites Melting relations of rocks at 1 atmosphere and 9 kbar Analyses for use in exercises Anhydrous melt compositions for Picture Gorge tholeiite Compositions and CIPW norms of experimentally melted rocks Glass representing liquid in equilibrium with Fo + Opx + Cpx + V at 1050 C and 20 kbar 265 loa Composition of rocks used by Mysen and Boettcher (1975a, b, ) 10.5 Compositions of partial melts formed from rocks Band E of Table 10.4 at various pressures, temperatures and values ofx H Details of phenocrysts in pumice blocks of Aso III ash-flow sheet Analyses of glasses (recalculated free of H 2 0 and CO 2) from Aso III pumice blocks Compositions of phenocrysts in Shamsan caldera sequence lavas Typical trace element distribution coefficients Ionic radius and charge of some important major and trace elements Radioactive decay schemes used in petrology Generalised initial 87Sr /86Sr ratios of igneous rocks Stable isotopes of light elements A 396 AU Nomenclature of rocks in the Q-A-P and A-P-F triangles 401

Geophysical Interpretation using Integral Equations

Geophysical Interpretation using Integral Equations Geophysical Interpretation using Integral Equations Geophysical Interpretation using Integral Equations L. ESKOLA Head of the Geophysics Department, Geological Survey of Finland 1~lll SPRINGER-SCIENCE+BUSINESS

More information

GY303 Igneous & Metamorphic Petrology. Lecture 7: Magma Sources and Tectonic Environments

GY303 Igneous & Metamorphic Petrology. Lecture 7: Magma Sources and Tectonic Environments GY303 Igneous & Metamorphic Petrology Lecture 7: Magma Sources and Tectonic Environments Factors controlling Magma production Source rock composition Amount of fluids, especially H 2 O Pressure (Depth)

More information

C = 3: Ternary Systems: Example 1: Ternary Eutectic

C = 3: Ternary Systems: Example 1: Ternary Eutectic Phase Equilibrium C = 3: Ternary Systems: Example 1: Ternary Eutectic Adding components, becomes increasingly difficult to depict 1-C: P - T diagrams easy 2-C: isobaric T-X, isothermal P-X 3-C:?? Still

More information

Differentiation of Magmas By Fractional Crystallization

Differentiation of Magmas By Fractional Crystallization Wirth Magmatic Differentiation Using M&M s 1 HANDOUT Differentiation of Magmas By Fractional Crystallization Objective The objective of this exercise is to gain first-hand knowledge of the process of magmatic

More information

TRACE ELEMENTS IN MAGMAS

TRACE ELEMENTS IN MAGMAS TRACE ELEMENTS IN MAGMAS A Theoretical Treatment Studying the distribution of certain elements, present in very low concentrations in igneous and metamorphic rocks, can yield important clues about the

More information

Partial melting of mantle peridotite

Partial melting of mantle peridotite Partial melting of mantle peridotite 1100 1200 1300 1400 1500 (TºC) Depth (km) 50 100 150 Plag lherzolite (ol-opx-cpx-pl) Spinel lherzolite (Ol-opx-cpx-sp) Garnet lherzolite (Ol-opx-cpx-gar) Graphite Diamond

More information

Differentiation of Magmas By Fractional Crystallization Modified from Karl Wirth, rev. July 2011

Differentiation of Magmas By Fractional Crystallization Modified from Karl Wirth, rev. July 2011 M&M s Magma Chamber 1 Differentiation of Magmas By Fractional Crystallization Modified from Karl Wirth, rev. July 2011 Objective The objective of this exercise is to gain first-hand knowledge of the process

More information

Finite Element Analysis for Heat Transfer. Theory and Software

Finite Element Analysis for Heat Transfer. Theory and Software Finite Element Analysis for Heat Transfer Theory and Software Hou-Cheng Huang and Asif S. Usmani Finite Element Analysis for Heat Transfer Theory and Software With 62 Figures Springer-Verlag London Berlin

More information

DIFFERENTIATION OF MAGMAS BY FRACTIONAL CRYSTALLIZATION THE M&M MAGMA CHAMBER

DIFFERENTIATION OF MAGMAS BY FRACTIONAL CRYSTALLIZATION THE M&M MAGMA CHAMBER Geol 2312 Igneous and Metamorphic Petrology Spring 2009 Name DIFFERENTIATION OF MAGMAS BY FRACTIONAL CRYSTALLIZATION THE M&M MAGMA CHAMBER Objective: This exercise is intended to improve understanding

More information

Universitext. Series Editors:

Universitext. Series Editors: Universitext Universitext Series Editors: Sheldon Axler San Francisco State University, San Francisco, CA, USA Vincenzo Capasso Università degli Studi di Milano, Milan, Italy Carles Casacuberta Universitat

More information

LAB 9: ULTRAMAFIC ROCKS, CUMULATES AND MELT SOURCES

LAB 9: ULTRAMAFIC ROCKS, CUMULATES AND MELT SOURCES Geology 316 (Petrology) (03/26/2012) Name LAB 9: ULTRAMAFIC ROCKS, CUMULATES AND MELT SOURCES INTRODUCTION Ultramafic rocks are igneous rocks containing less than 10% felsic minerals (quartz + feldspars

More information

Structure and Properties of Oriented Polymers

Structure and Properties of Oriented Polymers Structure and Properties of Oriented Polymers Structure and Properties of Oriented Polymers Edited by 1. M. Ward IRC in Polymer Science and Technology Universities of Leeds, Bradford and Durham UK I uni

More information

EARTH 331: Course Syllabus VOLCANOLOGY and IGNEOUS PETROLOGY. EIT 2047 Office Hours: meetings by appointment

EARTH 331: Course Syllabus VOLCANOLOGY and IGNEOUS PETROLOGY. EIT 2047 Office Hours: meetings by appointment EARTH 331: Course Syllabus VOLCANOLOGY and IGNEOUS PETROLOGY Instructor: Lab Instructor: Teaching Assistant: Katherine LaHay EIT 2047 klahay@uwaterloo.ca Office Hours: meetings by appointment Schedule:

More information

P.M. Cohn. Basic Algebra. Groups, Rings and Fields. m Springer

P.M. Cohn. Basic Algebra. Groups, Rings and Fields. m Springer Basic Algebra P.M. Cohn Basic Algebra Groups, Rings and Fields m Springer P.M. Cohn, MA, PhD, FRS Department of Mathematics, University College London, Gower Street, London WC1E 6BT, UK British Library

More information

Exam I. 1. (10 points) Give the following optical properties for the minerals listed below.

Exam I. 1. (10 points) Give the following optical properties for the minerals listed below. GLY306 Petrology Exam I 1. (10 points) Give the following optical properties for the minerals listed below. Color/pleochroism Extinction angle Cleavage angle Twining Refractive index Hornblende Plagioclase

More information

Astronomy with a Budget Telescope

Astronomy with a Budget Telescope Astronomy with a Budget Telescope Springer-Verlag London Ltd. Patrick Moore and John Watson Astro omy w h a Budget elescope With 100 Figures, 98 in colour, Springer British Library Cataloguing in Publication

More information

Minerals, Rocks and Inorganic Materials

Minerals, Rocks and Inorganic Materials Minerals, Rocks and Inorganic Materials Monograph Series of Theoretical and Experimental Studies 5 Edited by W. von Engelhardt, Tiibingen. T. Hahn, Aachen R. Roy, University Park, Pa.. P. J. Wyllie, Chicago,

More information

Practical Astronomy. Springer-Verlag London Ltd.

Practical Astronomy. Springer-Verlag London Ltd. Practical Astronomy Springer-Verlag London Ltd. Other titles in this series The Modern Amateur Astronomer Patrick Moore (Ed.) Telescopes and Techniques: An Introduction to Practical Astronomy C. R. Kitchin

More information

Origin of Basaltic Magma. Geology 346- Petrology

Origin of Basaltic Magma. Geology 346- Petrology Origin of Basaltic Magma Geology 346- Petrology 2 principal types of basalt in the ocean basins Tholeiitic Basalt and Alkaline Basalt Table 10-1 Common petrographic differences between tholeiitic and alkaline

More information

Name Petrology Spring 2006 Igneous rocks lab Part II Hand samples of igneous rocks Due Tuesday 3/7

Name Petrology Spring 2006 Igneous rocks lab Part II Hand samples of igneous rocks Due Tuesday 3/7 Igneous rocks lab Part II Hand samples of igneous rocks Due Tuesday 3/7 1. Use the color index and density of the rock to establish whether it is felsic, intermediate, mafic, or ultramafic. 2. Determine

More information

On Normalized Integral Table Algebras (Fusion Rings)

On Normalized Integral Table Algebras (Fusion Rings) On Normalized Integral Table Algebras (Fusion Rings) For further volumes: www.springer.com/series/6253 Algebra and Applications Volume 16 Series Editors: Alice Fialowski Eötvös Loránd University, Budapest,

More information

12 Chemistry (Mg,Fe) 2 SiO 4 Olivine is forms what is called an isomorphous solid solution series that ranges between two end members: Forsterite Mg

12 Chemistry (Mg,Fe) 2 SiO 4 Olivine is forms what is called an isomorphous solid solution series that ranges between two end members: Forsterite Mg 11 Olivine Structure Olivine is a common green or brown rock forming minerals which consists of a solid-solution series between Forsterite (Fo) and Fayalite (Fa). It is an orthorhombic orthosilicate with

More information

Electrical and Magnetic Methods of Non-destructive Testing

Electrical and Magnetic Methods of Non-destructive Testing Electrical and Magnetic Methods of Non-destructive Testing NON-DESTRUCTIVE EVALUATION SERIES Non-destructive evaluation now has a central place in modem technology both as a means of evaluating materials

More information

Introduction to CLASSICAL MECHANICS

Introduction to CLASSICAL MECHANICS Introduction to CLASSICAL MECHANICS Introduction to CLASSICAL MECHANICS A.P. FRENCH Massachusetts Institute oj Technology M.G. EBISON The Institute oj Physics, London KLUWER ACADEMIC PUBLISHERS DORDRECHT

More information

Igneous and Metamorphic Rock Forming Minerals. Department of Geology Mr. Victor Tibane SGM 210_2013

Igneous and Metamorphic Rock Forming Minerals. Department of Geology Mr. Victor Tibane SGM 210_2013 Igneous and Metamorphic Rock Forming Minerals Department of Geology Mr. Victor Tibane 1 SGM 210_2013 Grotzinger Jordan Understanding Earth Sixth Edition Chapter 4: IGNEOUS ROCKS Solids from Melts 2011

More information

How 2 nd half labs will work

How 2 nd half labs will work How 2 nd half labs will work Continue to use your mineral identification skills Learn to describe, classify, interpret rock hand samples: Igneous sedimentary metamorphic volcanic plutonic (1 week) (1 wk)

More information

ORE MICROSCOPY AND ORE PETROGRAPHY

ORE MICROSCOPY AND ORE PETROGRAPHY >...- ORE MICROSCOPY AND ORE PETROGRAPHY Second Edition JAMES R. CRAIG Department of Geological Sciences Virginia Polytechnic Institute and State University Blacksburg, Virginia DAVID J. VAUGHAN Department

More information

Earth Life System. An Introduction to the

Earth Life System. An Introduction to the An Introduction to the Earth Life System This undergraduate textbook brings together Earth and biological sciences to explore the co-evolution of the Earth and life over geological time. It examines the

More information

A. One component system (c = 1)

A. One component system (c = 1) A. One component system (c = 1) Example: SiO 2 system. Since all phases in this system have the same composition, there are no compositional variables to consider. Phase equilibria can be shown completely

More information

Lecture 25 Subduction Related Magmatism

Lecture 25 Subduction Related Magmatism Lecture 25 Subduction Related Magmatism Monday, May 2 nd 2005 Subduction Related Magmatism Activity along arcuate volcanic chains along subduction zones Distinctly different from the mainly basaltic provinces

More information

Block: Igneous Rocks. From this list, select the terms which answer the following questions.

Block: Igneous Rocks. From this list, select the terms which answer the following questions. Geology 12 Name: Mix and Match: Igneous Rocks Refer to the following list. Block: porphyritic volatiles mafic glassy magma mixing concordant discontinuous reaction series igneous vesicular partial melting

More information

GEOL 2312 Igneous and Metamorphic Petrology Spring 2016 Score / 58. Midterm 1 Chapters 1-10

GEOL 2312 Igneous and Metamorphic Petrology Spring 2016 Score / 58. Midterm 1 Chapters 1-10 GEOL 2312 Igneous and Metamorphic Petrology Name KEY Spring 2016 Score / 58 Midterm 1 Chapters 1-10 1) Name two things that petrologists want to know about magmas (1 pt) Formation, source, composition,

More information

Petrology. Petrology: the study of rocks, especially aspects such as physical, chemical, spatial and chronoligic. Associated fields include:

Petrology. Petrology: the study of rocks, especially aspects such as physical, chemical, spatial and chronoligic. Associated fields include: Petrology Petrology: the study of rocks, especially aspects such as physical, chemical, spatial and chronoligic. Associated fields include: Petrography: study of description and classification of rocks

More information

GEOL 3313 Petrology of Igneous and Metamorphic Rocks Study Guide for Final Examination Glen Mattioli

GEOL 3313 Petrology of Igneous and Metamorphic Rocks Study Guide for Final Examination Glen Mattioli GEOL 3313 Petrology of Igneous and Metamorphic Rocks Study Guide for Final Examination Glen Mattioli Chapter 5: Crystal-Melt phase diagrams Effect of water pressure on feldspar stability Hypersolvus vs.

More information

Geology 214 Optical Mineralogy, Introductory Petrology and Isotope Geology

Geology 214 Optical Mineralogy, Introductory Petrology and Isotope Geology Geology 214 Optical Mineralogy, Introductory Petrology and Isotope Geology 1. GENERAL INFORMATION Lecturer: Contact Details: Consultation: Course Description: Class Timetable: Dr. Jodie Miller, ph (021)

More information

PETROGENESIS OF A SERIES OF MAFIC SHEETS WITHIN THE VINALHAVEN PLUTON, VINALHAVEN ISLAND, MAINE

PETROGENESIS OF A SERIES OF MAFIC SHEETS WITHIN THE VINALHAVEN PLUTON, VINALHAVEN ISLAND, MAINE PETROGENESIS OF A SERIES OF MAFIC SHEETS WITHIN THE VINALHAVEN PLUTON, VINALHAVEN ISLAND, MAINE DANIEL HAWKINS Western Kentucky University Research Advisor: Andrew Wulff INTRODUCTION Round Point, in the

More information

Powder Surface Area and Porosity

Powder Surface Area and Porosity Powder Surface Area and Porosity Powder Technology Series EDITED BY BRIAN SCARLETI Delft University of Technology The Netherlands Many materials exist in the form of a disperse system, for example powders,

More information

Introductory Statement:

Introductory Statement: The use of visualization and sketches of thin sections to encourage a better understanding of phase diagrams: Binary and ternary phase diagram exercises Jennifer M. Wenner Drew S. Coleman Introductory

More information

2-C Eutectic Systems

2-C Eutectic Systems Phase Equilibrium 2-C Eutectic Systems Example: Diopside - Anorthite No solid solution * For system at this T, X, phase(s) plot where? Fig. 6.11. Isobaric T-X phase diagram at atmospheric pressure. After

More information

جامعة الملك سعود كلية العلوم قسم الجيولوجيا والجيوفيزياء

جامعة الملك سعود كلية العلوم قسم الجيولوجيا والجيوفيزياء King Saud University College of Sciences جامعة الملك سعود كلية العلوم قسم الجيولوجيا والجيوفيزياء Geology and geophysics Department Summer Course Igneous Petrology 32 Geo Course Academic Year 3-32H (200

More information

Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100

Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100 Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100 Ray Rector - Instructor Major Concepts 1) Igneous rocks form directly from the crystallization of a magma or lava 2)

More information

Earth Science 232 Petrography

Earth Science 232 Petrography Earth Science 232 Petrography Course notes by Shaun Frape and Alec Blyth Winter 2002 1 Petrology - Introduction Some Definitions Petra Greek for rock Logos Greek for disclosure or explanation Petrology

More information

Petrology. Petrology: the study of rocks, especially aspects such as physical, chemical, spatial and chronoligic. Classification:

Petrology. Petrology: the study of rocks, especially aspects such as physical, chemical, spatial and chronoligic. Classification: Petrology Petrology: the study of rocks, especially aspects such as physical, chemical, spatial and chronoligic. Associated fields include: Petrography: study of description and classification of rocks

More information

UNIVERSITY OF EDINBURGH. College of Science and Engineering School of GeoSciences. Earth Materials UO4824 DEGREE EXAMINATION (MOCK) xxxxxxxxxxxxxxxxx

UNIVERSITY OF EDINBURGH. College of Science and Engineering School of GeoSciences. Earth Materials UO4824 DEGREE EXAMINATION (MOCK) xxxxxxxxxxxxxxxxx UNIVERSITY OF EDINBURGH College of Science and Engineering School of GeoSciences Earth Materials UO4824 DEGREE EXAMINATION (MOCK) xxxxxxxxxxxxxxxxxxxx xxxxxxxxxxxxxxxxxxxxxx Chairman: External Examiners:

More information

EPS 50 Lab 2: Igneous Rocks Grotzinger and Jordan, Chapter 4

EPS 50 Lab 2: Igneous Rocks Grotzinger and Jordan, Chapter 4 Name: EPS 50 Lab 2: Igneous Rocks Grotzinger and Jordan, Chapter 4 Introduction In the previous lab, we learned about mineral characteristics, properties and identities as well as the three basic rock

More information

COURSE INFORMATION. NAME OF THE SUBJECT: Petrology of igneous and metamorphic rocks TEACHING STAFF

COURSE INFORMATION. NAME OF THE SUBJECT: Petrology of igneous and metamorphic rocks TEACHING STAFF COURSE INFORMATION NAME OF THE SUBJECT: Petrology of igneous and metamorphic rocks Code number: 757609217 Degree in Geology Academic Year: 2016-2017 Foundational/Elective/Compulsory course. 3 rd year Second

More information

INTRODUCTION TO SOL-GEL PROCESSING

INTRODUCTION TO SOL-GEL PROCESSING INTRODUCTION TO SOL-GEL PROCESSING THE KLUWER INTERNATIONAL SERIES in SOL-GEL PROCESSING: TECHNOLOGY AND APPLICATIONS Consulting Editor Lisa Klein Rutgers, the State University of New Jersey INTRODUCTION

More information

Rocks: Materials of the Solid Earth

Rocks: Materials of the Solid Earth 1 Rocks: Materials of the Solid Earth Presentation modified from: Instructor Resource Center on CD-ROM, Foundations of Earth Science,, 4 th Edition, Lutgens/Tarbuck, Rock Cycle Igneous Rocks Today 2 Rock

More information

WORKED EXAMPLES IN X-RAY ANALYSIS

WORKED EXAMPLES IN X-RAY ANALYSIS WORKED EXAMPLES IN X-RAY ANALYSIS PHILIPS TECHNICAL LIBRARY WORKED EXAMPLES IN X-RAY ANALYSIS R. JENKINS J.L. DE VRIES Springer Science+Business Media, LLC Springer Science+Business Media New York 1970

More information

Rare Earth Elements in some representative arc lavas

Rare Earth Elements in some representative arc lavas Rare Earth Elements in some representative arc lavas Low-K (tholeiitic), Medium-K (calc-alkaline), and High-K basaltic andesites and andesites. A typical N-MORB pattern is included for reference Notes:

More information

EARTH SCIENCES 3313A IGNEOUS PETROLOGY

EARTH SCIENCES 3313A IGNEOUS PETROLOGY EARTH SCIENCES 3313A IGNEOUS PETROLOGY Fall 2014 Instructor: Dr. Audrey Bouvier Office: B&GS 1040 Email: audrey.bouvier@uwo.ca Tel: 519 661 2111, ext: 88516 Office hours: Tuesdays 3-5pm, or by appointment

More information

Lecture 36. Igneous geochemistry

Lecture 36. Igneous geochemistry Lecture 36 Igneous geochemistry Reading - White Chapter 7 Today 1. Overview 2. solid-melt distribution coefficients Igneous geochemistry The chemistry of igneous systems provides clues to a number of important

More information

Convective Heat Transfer

Convective Heat Transfer Convective Heat Transfer Solved Problems Michel Favre-Marinet Sedat Tardu This page intentionally left blank Convective Heat Transfer This page intentionally left blank Convective Heat Transfer Solved

More information

Lecture 3 Rocks and the Rock Cycle Dr. Shwan Omar

Lecture 3 Rocks and the Rock Cycle Dr. Shwan Omar Rocks A naturally occurring aggregate of one or more minerals (e.g., granite), or a body of non-crystalline material (e.g., obsidian glass), or of solid organic material (e.g., coal). Rock Cycle A sequence

More information

Sphene (Titanite) Plane polarized light. Honey brown/orange Wedge-shaped crystals

Sphene (Titanite) Plane polarized light. Honey brown/orange Wedge-shaped crystals Sphene (Titanite) Plane polarized light Honey brown/orange Wedge-shaped crystals Sphene (Titanite) Crossed nicols High-order, washedout interference colors (light orange) #1 Rule for (Heavy) Radiogenic

More information

GLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition

GLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition Grotzinger Jordan Understanding Earth Sixth Edition Chapter 4: IGNEOUS ROCKS Solids from Melts 2011 by W. H. Freeman and Company Chapter 4: Igneous Rocks: Solids from Melts 1 About Igneous Rocks Igneous

More information

12. Data from Ito et al. (1987) Chemical Geology, 62, ; Figure ; and LeRoex et al. (1983) J. Petrol., 24,

12. Data from Ito et al. (1987) Chemical Geology, 62, ; Figure ; and LeRoex et al. (1983) J. Petrol., 24, Announcements Reading for Wed: p.363-399!!! p.362-366; p.373-378; p.383-386; p.392-394; p.395-399 Last lecture on Wednesday Bring food for pizza party Bring class notes, labs, book N-MORBs: 87 Sr/ 86 Sr

More information

Petrology of the metamorphic rocks

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.

More information

GEOLOGY. Subject : GEOLOGY (For under graduate student.) Paper No. : Paper 02 Introduction to Geology 02

GEOLOGY. Subject : GEOLOGY (For under graduate student.) Paper No. : Paper 02 Introduction to Geology 02 GEOLOGY Subject : GEOLOGY (For under graduate student.) Paper No. : Paper 02 Introduction to Geology 02 Topic No. & Title : 37 Magma Bowen Series (Part 01) Academic Script What is Igneous Petrology? Igneous

More information

Trace Elements. Today s lecture

Trace Elements. Today s lecture Trace Elements 300 Ni 200 ppm 100 0 300 Zr 200 100 0 40 50 60 70 80 SiO 2 wt. % Updates: M&M due date: Tuesday Today s lecture Topics: Trace element compositions Trace element behavior Partitioning Spider(

More information

Classification and Origin of Granites. A Multi-faceted Question

Classification and Origin of Granites. A Multi-faceted Question Classification and Origin of Granites A Multi-faceted Question What is a granite? IUGS classification Based on Modal Mineralogy Plutonic rock with less than 90% mafic minerals Alkali Granite Granite Quartz

More information

Archean Terranes. Archean Rocks. Southeastern Africa. West Greenland. Kaapvaal Craton. Ancient Gneiss Complex

Archean Terranes. Archean Rocks. Southeastern Africa. West Greenland. Kaapvaal Craton. Ancient Gneiss Complex Archean Terranes Archean Rocks Chapter 15A >2.5 Gy old Younger supracrustal sequences Greenstone belts Calc-alkaline metavolcanic rocks Older gneiss complexes Quartzo-feldspathic rocks Tonalites and migmatites

More information

23/9/2013 ENGINEERING GEOLOGY. Chapter 2: Rock classification:

23/9/2013 ENGINEERING GEOLOGY. Chapter 2: Rock classification: ENGINEERING GEOLOGY Chapter 2: Rock classification: ENGINEERING GEOLOGY Chapter 1.0: Introduction to engineering geology Chapter 2.0: Rock classification Igneous rocks Sedimentary rocks Metamorphic rocks

More information

FOUNDATION SCIENCE FOR ENGINEERS

FOUNDATION SCIENCE FOR ENGINEERS FOUNDATION SCIENCE FOR ENGINEERS Other titles of interest to engineers Dynamics G.E. Drabble Electric Circuits P. Silvester Electromagnetism R.G. Powell Engineering Mathematics, fourth edition K.A. Stroud

More information

9/4/2015. Feldspars White, pink, variable Clays White perfect Quartz Colourless, white, red, None

9/4/2015. Feldspars White, pink, variable Clays White perfect Quartz Colourless, white, red, None ENGINEERING GEOLOGY Chapter 1.0: Introduction to engineering geology Chapter 2.0: Rock classification Igneous rocks Sedimentary rocks Metamorphic rocks Chapter 3.0: Weathering & soils Chapter 4.0: Geological

More information

CHAPTER ROCK WERE FORMED

CHAPTER ROCK WERE FORMED HOW CHAPTER 3 ROCK WERE FORMED 1 I. Modern geology- 1795 A. James Hutton- 1. uniformitarianism- "the present is the key to the past" a. b. the geologic processes now at work were also active in the past

More information

CHAPTER ROCK WERE FORMED

CHAPTER ROCK WERE FORMED HOW CHAPTER 5 ROCK WERE FORMED 1 I. Modern geology- 1795 A. James Hutton- 1. uniformitarianism- "the present is the key to the past" a. b. the geologic processes now at work were also active in the past

More information

Research Techniques for High Pressure and High Temperature

Research Techniques for High Pressure and High Temperature Research Techniques for High Pressure and High Temperature Research Techniques for High Pressure and High Temperature Edited by Gene C. Ulmer Springer-Verlag New York Heidelberg Berlin 1971 All rights

More information

TWO COMPONENT (BINARY) PHASE DIAGRAMS. Experimental Determination of 2-Component Phase Diagrams

TWO COMPONENT (BINARY) PHASE DIAGRAMS. Experimental Determination of 2-Component Phase Diagrams Page 1 of 12 EENS 211 Earth Materials Tulane University Prof. Stephen A. Nelson TWO COMPONENT (BINARY) PHASE DIAGRAMS This document last updated on 08-Oct-2003 Experimental Determination of 2-Component

More information

Lab 3 - Identification of Igneous Rocks

Lab 3 - Identification of Igneous Rocks Lab 3 - Identification of Igneous Rocks Page - 1 Introduction A rock is a substance made up of one or more different minerals. Thus an essential part of rock identification is the ability to correctly

More information

Magma Formation and Behavior

Magma Formation and Behavior Magma Formation and Behavior Questions What causes mantle rock to melt, resulting in magma formation? Why is magma formation restricted to specific plate tectonic settings? Why are mafic (basaltic) magmas

More information

High-T T heating stage: : application for igneous petrogenesis and mantle processes - melt inclusions as key tools -

High-T T heating stage: : application for igneous petrogenesis and mantle processes - melt inclusions as key tools - High-T T heating stage: : application for igneous petrogenesis and mantle processes - melt inclusions as key tools - SZABÓ, Csaba Lithosphere Fluid Research Lab (LRG), Department of Petrology and Geochemistry,

More information

Triangular Diagrams. 1. On the diagram above, plot the following (mostly mineral) compositions: silicon quartz corundum kyanite

Triangular Diagrams. 1. On the diagram above, plot the following (mostly mineral) compositions: silicon quartz corundum kyanite Triangular Diagrams Note: For this exercise, everything is plotted using mole%. Sometimes it is done with wt% but that just adds unnecessary complications. 1. On the diagram above, plot the following (mostly

More information

Feldspars. Structure. The feldspars are by far the most abundant group of minerals and are found in igneous, metamorphic and many sedimentary rocks.

Feldspars. Structure. The feldspars are by far the most abundant group of minerals and are found in igneous, metamorphic and many sedimentary rocks. Feldspars The feldspars are by far the most abundant group of minerals and are found in igneous, metamorphic and many sedimentary rocks. Structure Felsdpars are framework silicates where each silica tetrahedra

More information

GIS AND TERRITORIAL INTELLIGENCE. Using Microdata. Jean Dubé and Diègo Legros

GIS AND TERRITORIAL INTELLIGENCE. Using Microdata. Jean Dubé and Diègo Legros GIS AND TERRITORIAL INTELLIGENCE Spatial Econometrics Using Microdata Jean Dubé and Diègo Legros Spatial Econometrics Using Microdata To the memory of Gilles Dubé. For Mélanie, Karine, Philippe, Vincent

More information

Minoru Ozima. Geohistory. Global Evolution of the Earth. English by Judy Wakabayashi. Springer-Verlag Berlin Heidelberg New York London Paris Tokyo

Minoru Ozima. Geohistory. Global Evolution of the Earth. English by Judy Wakabayashi. Springer-Verlag Berlin Heidelberg New York London Paris Tokyo Minoru Ozima Geohistory Global Evolution of the Earth English by Judy Wakabayashi Springer-Verlag Berlin Heidelberg New York London Paris Tokyo Professor Dr. MINORU OZIMA Geophysical Institute University

More information

N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0

N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0 N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0 is initial number of parents, D* is number of radiogenic daughter atoms, and λ is the decay

More information

UNDERSTANDING MINERAL DEPOSITS

UNDERSTANDING MINERAL DEPOSITS UNDERSTANDING MINERAL DEPOSITS U nderstanding Mineral Deposits by Kula c. Misra Department of Geological Sciences, The University oftennessee, Knoxville, U.S.A. SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. A

More information

Essentials of Geology, 11e

Essentials of Geology, 11e Essentials of Geology, 11e Igneous Rocks and Intrusive Activity Chapter 3 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Characteristics

More information

Reliability Evaluation of Engineering Systems:

Reliability Evaluation of Engineering Systems: Reliability Evaluation of Engineering Systems: Concepts and Techniques Roy Billinton PhD, DSc, FEIC, FRSC, FIEEE, PE c. J. MacKenzie Professor of Electrical Engineering University of Saskatchewan and Ronald

More information

THE BOUNDARY ELEMENT METHOD

THE BOUNDARY ELEMENT METHOD THE BOUNDARY ELEMENT METHOD SOLID MECHANICS AND ITS APPLICATIONS Volume 27 Series Editor: G.M.L. GLADWELL Solid Mechanics Division, Faculty of Engineering University of Waterloo Waterloo, Ontario, Canada

More information

EESC 4701: Igneous and Metamorphic Petrology IGNEOUS ROCK CLASSIFICATION LAB 2 HANDOUT

EESC 4701: Igneous and Metamorphic Petrology IGNEOUS ROCK CLASSIFICATION LAB 2 HANDOUT EESC 4701: Igneous and Metamorphic Petrology IGNEOUS ROCK CLASSIFICATION LAB 2 HANDOUT Sources: University of Washington, Texas A&M University, University of Southern Alabama What is an igneous rock (a

More information

To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle

To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle Bell Ringer Name the 3 types of rock. Is one type of rock able to change into a different

More information

Selection Methods in Plant Breeding

Selection Methods in Plant Breeding Selection Methods in Plant Breeding PLANT BREEDING SERIES Edited by Professor P.D.S. Caligari Head of the Department of Agricultural Botany The University of Reading, UK Modem plant breeders need to have

More information

Chapter 4 Rocks & Igneous Rocks

Chapter 4 Rocks & Igneous Rocks Chapter 4 Rocks & Igneous Rocks Rock Definition A naturally occurring consolidated mixture of one or more minerals e.g, marble, granite, sandstone, limestone Rock Definition Must naturally occur in nature,

More information

Igneous Rocks. Igneous Rocks - 1. Environment of Formation - Magma - Plutonic - rock that formed within the Earth. Intrusive - Earth s crust.

Igneous Rocks. Igneous Rocks - 1. Environment of Formation - Magma - Plutonic - rock that formed within the Earth. Intrusive - Earth s crust. Name: Date: Period: Minerals and Rocks The Physical Setting: Earth Science CLASS NOTES - Methods to classify igneous rocks: 1. Environment of Formation - Magma - Plutonic - rock that formed within the

More information

1 - C Systems. The system H 2 O. Heat an ice at 1 atm from-5 to 120 o C. Heat vs. Temperature

1 - C Systems. The system H 2 O. Heat an ice at 1 atm from-5 to 120 o C. Heat vs. Temperature 1 - C Systems The system H 2 O Heat an ice at 1 atm from-5 to 120 o C Heat vs. Temperature Fig. 6.7. After Bridgman (1911) Proc. Amer. Acad. Arts and Sci., 5, 441-513; (1936) J. Chem. Phys., 3, 597-605;

More information

Igneous Rock. Magma Chamber Large pool of magma in the lithosphere

Igneous Rock. Magma Chamber Large pool of magma in the lithosphere Igneous Rock Magma Molten rock under the surface Temperature = 600 o 1400 o C Magma Chamber Large pool of magma in the lithosphere Magma chamber - most all magma consists of silicon and oxygen (silicate)

More information

13. PETROLOGY OF BASALTS FROM DEEP SEA DRILLING PROJECT, LEG 38

13. PETROLOGY OF BASALTS FROM DEEP SEA DRILLING PROJECT, LEG 38 . PETROLOGY OF BASALTS FROM DEEP SEA DRILLING PROJECT, LEG W.I. Ridley, M.R. Perfit, and ML. Adams, LamontDoherty Geological Observatory, Columbia University, Palisades, New York INTRODUCTION We have determined

More information

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

Name Class Date STUDY GUIDE FOR CONTENT MASTERY Igneous Rocks What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. extrusive igneous rock intrusive

More information

Worked Example of Batch Melting: Rb and Sr

Worked Example of Batch Melting: Rb and Sr Worked Example of Batch Melting: Rb and Sr Basalt with the mode: Table 9.2. Conversion from mode to weight percent Mineral Mode Density Wt prop Wt% ol 15 3.6 54 0.18 cpx 33 3.4 112.2 0.37 plag 51 2.7 137.7

More information

A Rock is a solid aggregate of minerals.

A Rock is a solid aggregate of minerals. Quartz A Rock is a solid aggregate of minerals. Orthoclase Feldspar Plagioclase Feldspar Biotite Four different minerals are obvious in this piece of Granite. The average automobile contains: Minerals

More information

OUTCOMES BASED LEARNING MATRIX. Course: Physical Geology Department: _Physical Science. Study the text and lecture material

OUTCOMES BASED LEARNING MATRIX. Course: Physical Geology Department: _Physical Science. Study the text and lecture material OUTCOMES BASED LEARNING MATRIX Course: Physical Geology Department: _Physical Science Physical Geology This course is intended to acquaint students with the physical structure of the Earth, the nature

More information

Notes for Use of the Cpx-Plag-Ol Thermobar Workbook Last Updated:

Notes for Use of the Cpx-Plag-Ol Thermobar Workbook Last Updated: Notes for Use of the Cpx-Plag-Ol Thermobar Workbook Last Updated: 7-22-05 Cpx-Plag-Ol Thermobar is an Excel workbook that can be used to calculate crystallization pressures and temperatures for clinopyroxene-

More information

Igneous Rocks of the Convergent Margins

Igneous Rocks of the Convergent Margins Page 1 of 10 EENS 2120 Petrology Prof. Stephen A. Nelson Tulane University Igneous Rocks of the This document last updated on 08-Feb-2011 The convergent plate margins are the most intense areas of active

More information

Happy Tuesday. Pull out a ½ sheet of paper

Happy Tuesday. Pull out a ½ sheet of paper Happy Tuesday Pull out a ½ sheet of paper 1. Physical properties of a mineral are predominantly related to 1. the external conditions of temperature, pressure, and amount of space available for growth.

More information

TEACHER BACKGROUND KNOWEDGE. Minerals, Rocks and the Rock Cycle

TEACHER BACKGROUND KNOWEDGE. Minerals, Rocks and the Rock Cycle TEACHER BACKGROUND KNOWEDGE Minerals, Rocks and the Rock Cycle Core Concepts Rocks in the Earth s crust vary in their form and structure based on process that made them. The constant changing of the form

More information

Lecture 6 - Igneous Rocks and Volcanoes

Lecture 6 - Igneous Rocks and Volcanoes Lecture 6 - Igneous Rocks and Volcanoes Learning objectives Understand and be able to predict where and why magma will be forming at different tectonic settings Understand the factors controlling magma

More information

Igneous & Metamorphic Petrology I LECTURE 11

Igneous & Metamorphic Petrology I LECTURE 11 Igneous & Metamorphic Petrology I LECTURE 11 The Earth s Mantle 1. Structure of the Earth A Reminder The velocities of seismic waves differ with the elastic properties and densities of rocks and allow

More information

Engineering Geology ECIV 2204

Engineering Geology ECIV 2204 Engineering Geology ECIV 2204 Instructor : Dr. Jehad Hamad 2017-2016 Chapter (3) Igneous Rocks Chapter 3: Rocks: Materials of the Solid Earth Igneous Rocks Chapter 3: Rocks: Materials of the Solid Earth

More information