GEOL 321 Structural Geology and Tectonics

Similar documents
Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.

Chapter 15 Structures

Geology for Engineers Rock Mechanics and Deformation of Earth Materials

Stress and Strain. Stress is a force per unit area. Strain is a change in size or shape in response to stress

Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name

Chapter Review USING KEY TERMS. asthenosphere uplift continental drift. known as. tectonic plates move. object. UNDERSTANDING KEY IDEAS

Captain s Tryouts 2017

Mountains are then built by deforming crust: Deformation & Mountain Building. Mountains form where stresses are high!

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building

UNIT 10 MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS

Plate Tectonics. entirely rock both and rock

Crustal Deformation. Earth Systems 3209

Deformation of Rocks. Orientation of Deformed Rocks

11.1 Rock Deformation

GENERAL GEOLOGY Fall Chapter 18: The Sea Floor. Partial Examination IV Study Guide Dr. Glen S. Mattioli

Chapter 10: Deformation and Mountain Building. Fig. 10.1

Provided by Tasa Graphic Arts, Inc. for An Introduction to Structural Methods DVD-ROM

Chapter 16. Mountain Building. Mountain Building. Mountains and Plate Tectonics. what s the connection?

Lecture Outline Friday March 2 thru Wednesday March 7, 2018

PHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION)

10. Paleomagnetism and Polar Wandering Curves.

What Causes Rock to Deform?

Exam Deformatie en Metamorfose van de Korst Educatorium zaal ALFA

Deformation: Modification of Rocks by Folding and Fracturing

Plate Tectonics - Demonstration

Structural Geology and Geology Maps Lab

Deformation of the Crust

Distribution of Continents Mid-ocean Ridges Trenches. Deformation Metamorphism Volcanism Earthquakes

Geologic Structures. Changes in the shape and/or orientation of rocks in response to applied stress

Lecture 6 Folds, Faults and Deformation Dr. Shwan Omar

Strike-Slip Faults. ! Fault motion is parallel to the strike of the fault.

Chapter. Graphics by Tasa Graphic Arts. Inc.

Staple this part to part one of lab 6 and turn in. Lab 6, part two: Structural geology (analysis)

CRUSTAL DEFORMATION. Chapter 10

Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS

CHAPTER Va : CONTINUOUS HETEROGENEOUS DEFORMATION

1. What is Wegener s theory of continental drift? 2. What were the 4 evidences supporting his theory? 3. Why wasn t Wegener s theory excepted?

FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC

Mohorovicic discontinuity separates the crust and the upper mantle.

Essentials of Geology, 11e

Unit 4 Lesson 3 Mountain Building. Copyright Houghton Mifflin Harcourt Publishing Company

Description of faults

Mountains and Mountain Building: Chapter 11

Lab 1: Plate Tectonics April 2, 2009

1. classic definition = study of deformed rocks in the upper crust

Earthquakes. Earthquakes are caused by a sudden release of energy

OCN 201: Seafloor Spreading and Plate Tectonics I

FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC

Do NOT open the test until instructed to do so.

Geology 101 Reading Guide for Plate Tectonics

Lecture 9 faults, folds and mountain building

Plate Tectonics. I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move

Whole Earth Structure and Plate Tectonics

Crustal Deformation Earth - Chapter Pearson Education, Inc.

Chapter 4 Section 3, 4. Deforming the Earth s Crust

Brittle Deformation. Earth Structure (2 nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm

Chapter. Mountain Building

Convergent plate boundary.

Unit 4 Lesson 7 Mountain Building

FORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.

EAS FINAL EXAM

Answers: Internal Processes and Structures (Isostasy)

December 21, Chapter 11 mountain building E.notebook. Feb 19 8:19 AM. Feb 19 9:28 AM

Part I. PRELAB SECTION To be completed before labs starts:

Physical Geology, 15/e

Introduction To Plate Tectonics Evolution. (Continents, Ocean Basins, Mountains and Continental Margins)

USU 1360 TECTONICS / PROCESSES

Name Student ID Exam 2c GEOL 1113 Fall 2009

DYNAMIC PLANET. Name: School:

Lecture 4.1 Continental Drift

How mountains are made. We will talk about valleys (erosion and weathering later)

Section 2: How Mountains Form

Geology 15 West Valley College. Exam IV: Sierra Nevada

GEOLOGIC MAPS PART II

Learning Objectives (LO) What we ll learn today:!

GEOL372: Week 5 Thrust fault systems. Contractional regimes

Forces That Shape Earth. How do continents move? What forces can change rocks? How does plate motion affect the rock cycle?

Lecture Outlines PowerPoint. Chapter 10 Earth Science, 12e Tarbuck/Lutgens

Faults, folds and mountain building

Introduction to Geology Spring 2008

Folds and Folding. Processes in Structural Geology & Tectonics. Ben van der Pluijm. WW Norton+Authors, unless noted otherwise 3/4/ :15

Directed Reading. Section: How Mountains Form MOUNTAIN RANGES AND SYSTEMS. Skills Worksheet

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent

Week: 4 5 Dates: 9/2 9/12 Unit: Plate Tectonics

1/27/2011 C H A P T E R 4 P L A T E T E C T O N I C S. Plate Tectonics. Highest pt=mt Everest, ft, 8848 m. Lowest pt. Marianas trench, -11,000 m

Plate Boundaries & Resulting Landforms

Material is perfectly elastic until it undergoes brittle fracture when applied stress reaches σ f

Exploring Inside the Earth

Course Title: Discipline: Geology Level: Basic-Intermediate Duration: 5 Days Instructor: Prof. Charles Kluth. About the course: Audience: Agenda:

5/24/2018. Plate Tectonics. A Scientific Revolution Unfolds

Earthquakes = shaking of Earth because of a rapid release of energy

UNIVERSITY OF PRETORIA Department of Geology STRUCTURAL GEOLOGY -GLY 254 SEMESTER EXAM

Chapter 7 Plate Tectonics

Contractional Tectonics: Convergence and Collision

Ch. 9 Review. Pgs #1-31 Write Questions and Answers

Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms.

GEOLOGY MEDIA SUITE Chapter 13

Plate Tectonics: A Scientific Revolution Unfolds

Section 3 Deforming Earth s Crust

Deformation and Structural Geology Course Profile i

Transcription:

GEOL 321 Structural Geology and Tectonics Geology 321 Structure and Tectonics will be given in Spring 2017. The course provides a general coverage of the structures produced by brittle and ductile rock deformation at scales from the hand-specimen to plate boundaries, and an insight into the relationships between the deformational structures and plate tectonic settings. The emphasis will be on the description and interpretation of structures seen in the field, and the course includes an introduction to the techniques of geological mapping in a structurally complex terrain, and the interpretation of geological maps and sections. Lab exercises will involve calculations and graphical exercises, but a basic math preparation is sufficient to follow the course. There will be two day trips and two weekend trips, including a mapping trip in the Inyo Mountains. The weekend trips are provisionally scheduled for February 24-27 and April 15-17: in both cases we will try to leave as early as we can on the Friday, and return late Sunday. The day trips will be scheduled on Thursdays, and will be arranged in class. Lectures (11.00-12.25 T, Th), Labs (TBA). 2 weekend field trips and 2 day trips. Assessment is based on lab assignments, field trip reports, and a final examination. Flow chart for course: Plate tectonics tectonic regimes structural geometry mechanics rheology fault rocks ductile structures mylonites rift zones strike-slip zones thrust belts. Schedule Classes start: Monday January 9 Martin Luther King s Birthday: Mon January 16 President s Day: Mon February 20 Spring Recess: March 12-19 Classes end: Friday April 28 Field exercise 1: Southern California tectonics (day trip, February) Field exercise 2: Death Valley (weekend trip February 24-27) Field exercise 3: Field methods in structural geology (day trip, March) Field exercise 4: Mapping in the Inyo Mtns (weekend trip, April 15-17). Note: the sequence of lectures and lab exercises shown below is provisional. There will be additional lectures and labs related to the field trips, and a review session at the end of the semester. Plate tectonics and tectonic regimes Reading: Davis & Reynolds chapter 10. Lecture 1: The Earth as a mechanical system. Heat flow and the global energy budget

Conduction and convection Compositional boundaries within the Earth Lithosphere and asthenosphere. Thermal and mechanical boundary layers. Decompression melting and the origin of the oceanic crust Isostasy, gravity and topography Lecture 2: Continental drift and plate tectonics Geometrical and geological evidence for continental drift Apparent polar wander paths Distribution of seismicity Sea-floor magnetic anomalies Geometrical concept of plate tectonics. Lab exercise 1: Introduction to geological maps Reading: Moores & Twiss, sections 5.1-5.5. Lecture 3: Divergent plate boundaries and transform faults Topographic and structural expression of mid-ocean ridges Subsidence history of oceanic lithosphere Magmatism at mid-ocean ridges Magmatic structure of oceanic crust as revealed in ophiolite sequences Kinematic behaviour of transform faults Seismicity and topographic expression of transform faults Lecture 4: Convergent plate boundaries Benioff seismic zones Surface structure: Accretionary wedge forearc basin magmatic arc back-arc Introceanic and continental arcs Continental collision zones Lab exercise 2: Introduction to geological maps (continued) Reading: Moores & Twiss, sections 7.1 7.4 Lecture 5: Geometrical aspects of plate motion Euler s theorem Relative velocities and poles of rotation Kinematic and geometrical characteristics of plate boundaries Triple junctions Lecture 6: Continental rift zones and the evolution of passive continental margins Structure of continental rifts. East African Rift as an example Initiation of continental breakup. Red Sea as an example Evolution of passive continental margins: Atlantic margin of eastern US as an example.

Lab exercise 3: Plate kinematics Structural Geometry Reading: Davis & Reynolds, p. 269-296 Lecture 7: Faulting Description of deformation in terms of geometry, kinematics, and dynamics. Geometrical description of faults. Slip and stratigraphic separation on faults. Methods for determining the slip vector on a fault. Lecture 8: Fault rocks and small-scale structures in fault zones. Fault rocks: fault breccia, cataclasite, mylonite, pseudotachylite Slickensides and slickenlines Gouge fabrics, Riedel shears Wear grooves, fibre lineations, solution grooves Sense of shear indicators in fault zones. Lab exercise 4: Day field trip and field-trip follow-up. Reading, week 5: Davis & Reynolds, p. 373-403 Lecture 9: Geometrical description of folds Fold hinge, axis, axial surface, fold crest Inclined folds and plunging folds Fold asymmetry, enveloping surface of a fold train Fold style: parallel, concentric, similar, kink geometries. Lecture 10: Folds and rock fabrics Axial plane cleavage in folds. Linear fabric elements in folds. Use of folds, cleavages and lineations in structural analysis Lab exercise 5: Introduction to the equal-area projection Introduction to Structural Mechanics Reading: Davis & Reynolds, p. 98-134 Lecture 11: Stress Force and stress Stress on a surface: tractions and the stress vector Stress field in 3-D; Principal stresses Hydrostatic and deviatoric stress Mohr equations and the Mohr construction for stress Lecture 12: Fracture mechanics The Coulomb fracture criterion.

Use of the Mohr construction to represent fracture mechanics Failure envelope Effect of fluid pressure on fracture Lab exercise 6: Geometrical analysis of folds Reading: Davis & Reynolds, p. 38-74 Lecture 13: Strain Displacement gradients, rotation, and strain. Elongation, stretch, shear strain, volumetric strain Incremental strain and strain-rate Lecture 14: Strain analysis Strain analysis using spherical objects Center-to-center method Rf/phi method Mohr construction for strain Strain analysis using deformed fossils Lab exercise 7: The Mohr construction for stress and its use in fracture mechanics Ductile deformation Reading: Davis & Reynolds, p. 143-149, 424-436, 456-471 Lecture 15: Ductile deformation Rheology Elastic, viscous and plastic deformation Rheological analogues Deformational mechanisms in rocks Lecture 16: Ductile deformational fabrics Planar deformational fabrics: cleavage, schistosity, gneissic foliation, mylonitic foliation, crenulation cleavage. Linear deformational fabrics: intersection lineation, stretching lineation, crenulation lineation. Lab exercise 8: Strain analysis Reading: Davis & Reynolds, p. 493-523, 404-413 Lecture 17: Ductile shear zones Boundary conditions limiting nature of flow in ductile shear zones Geometry of simple shear Foliation geometry in ductile shear zones Mylonites Sense of shear criteria in mylonites

Lecture 18: Mechanics of folding 1 Fold style in terms of the geometry of the folded layer Mechanical theory of buckle folding in single layers. Lab exercise 9: Day field trip and field trip follow up Lecture 21: Mechanics of folding 2 Folding in multilayers; flexural slip folds Kinks. Similar folds and flow folds Lecture 22: Analysis of polyphase deformation Superposed folds Interference structures Folded foliations and superposed foliations Folded lineations Lab exercise 10: Field trip follow up Tectonics Lecture 23: Tectonic styles in zones of strike-slip faulting Patterns of folds and faults in strike-slip fault zones Flower structures Releasing and restraining bends Pull-apart basins Vertical-axis rotations in in strike-slip fault zones Deep structure of strike-slip fault zones Lecture 24: Tectonic styles in zones of normal faulting Conjugate sets of normal faults Horst and graben structure Detachment faults Rotation of normal faults above listric faults and detachments Rolling hinge model for detachment faults Lab exercise 11: Structures and fabrics in rocks Lecture 23: Tectonic styles in zones of thrust faulting Thin-skinned and thick-skinned thrust belts Ramp and flat structures Ramp anticlines and footwall synclines Fault propagation folds Frontal imbricate fan

Duplex structure Culminations Backthrusts and pop-up structures Lecture 24: Construction and restoration of balanced sections Lab exercise 12: Construction and restoration of balanced sections FINAL EXAMINATION: Tues May 9, 11-1.