Fractures, Faults, & Friction

Slides:



Advertisements
Similar presentations
Relative dating.
Advertisements

Brittle deformation II
Structural Geology Crustal Deformation
Mechanics of Materials – MAE 243 (Section 002) Spring 2008
Stress and Deformation: Part I (D&R, ; ) The goal for today is to explore the stress conditions under which rocks fail (e.g., fracture),
Anderson’s theory of faulting
Relative Dating The Law of Superposition
Announcements Talk This Thurs. 4 pm, Rm. Haury Bldg. Rm 216, "Tertiary structural and stratigraphic evolution of the Greater Tucson area", by Jon Spencer.
Structural Geology: Deformation and Mountain Building
Geologic Maps and Structures Lab 2a Geology 208. Geologic Maps: Snoqualmie Pass.
Announcements This week's lab: 1-3 PM with Andrew McCarthy. Please come prepared with specific questions. There will be no lecture this Wednesday! Please.
The last of the CIRCULAR GRAPHS which will HAUNT YOU ALL QUARTER January 13, 2005 [Many thanks to H. Bob]
Joints and Shear Fractures
Announcements Field trip this Saturday to Cottonwood Canyon area 7:30 AM at loading dock. We will map some really cool stuff! Please review map symbols.
Supplemental Review and Exercises
Types of Metamorphism Regional metamorphism
EARS 5131 STUCTURE AND HYDROCARBON PROSPECTIVITY OF BASIN.
folded and disturbed layers
Rock Deformation Chapter 11, Section 1.
Folds, Faults, and Geologic Maps
Geologic Structures Physical Geology, Chapter 15
Folds Rocks are often bent into a series of wave-like undulations called folds Characteristics of folds Folds result from compressional stresses which.
1 THRUST FAULTS: ASSOCIATED STRUCTURES AND IMPLICATIONS IN HYDROCARBONS TRAPS James Moore Alex Nyombi Christian Hidalgo Adekunle Odutola STRUCTURE AND.
Crustal Deformation Structural Geology
Faults, Folds, and Landscapes
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Structural Geology.
II. Basic Techniques in Structural Geology
Integrating geologic maps with fault mechanics John Singleton, George Mason University NSF Cutting Edge Workshop 2012.
Contraction- Thrust FaultsEarth contraction: (strain-related term). Shortening in a direction set by the acting field stress. -accomodated by contractional.
This is the trace of the strain tensor. In general the trace of the strain tensor gives area change in 2-D and volume change in 3-D The principal axes.
Geologic Structure.
MECHANICS OF PLASTIC DEFORMATION > PLASTIC DEFORMATION IS BY FLOW; THE PROCESSES MAY BE: 1.INTERGRANULAR MOVEMENT A) DISPLACEMENT TAKES PLACE BETWEEN INDIVIDUAL.
STRESS, FAULTS, AND FOLDS. Deformation is the bending, tilting, and breaking of the Earth’s crust. Plate tectonics is the major cause of crustal deformation.
Lecture 2: Deformation, reference frame,
Geology Failure Models
Testing models – Structural restoration. Ben Peach’s field notebook: 1880s. Line-length balancing Area balancing.
2 Types.  Relative Dating  Absolute Dating  1. Law of superposition – youngest layer on top; oldest layer on bottom.
Brittle Deformation Remember that  is the angle between  3 and a plane.
STRUCTURAL GEOLOGY  PRIMARY & NON-TECTONIC STRUCTURES 1) PRINCIPLE OF ORIGINAL HORIZONTALITY (NICOLAS STENO ) – LAYERS OF SEDIMENTS ARE ORIGINALLY.
Geological time scale Deformed Laws and Principles.
Mohr-Coulomb failure Goal: To understand relationship between stress, brittle failure, and frictional faulting and to use this relationship to predict.
structural geology & mountain building
Structure An Introduction to Deformation. Standards Describe the composition and structure of Earth’s materials.
Presentation on Terminology and different types of Faults
Forces In Mountain Building
Mountain Building Folding and Faulting. Stress in the Crust Stress from plate motions causes crustal rocks to deform –Rocks near the surface are cool.
GEOTECHNICS AND APPLIED GEOLOGY
FOLDS, FAULTS AND GEOLOGIC MAPS
Faults III Lecture 29 Gly 326.
Lecture Outlines Physical Geology, 12/e
Eric H Christiansen.
Forces In Mountain Building
Ketobe Knob, UT.
Relative Dating.
FACULTY OF ENGINEERING TECHNOLOGY & RESEARCH
Fold Thrust Belts.
Field measurements Preparation to field work
Submition : geology Group:2.
Forces that cause deformation
Faults
GEOLOGICAL STRUCTURES
Earth Systems 3209 Unit 2: Relative Dating.
Structural Geology Structural geology is the study of rocks deformed by stress and strain This involves trying to understand stress and strain forces to.
Outline Terminology Ramp and Flat thrusts Animations
Relative Dating.
Deformations Folds Faults and Fractures Continental Collisions Crustal Fragments and Mountain Building CHARLITO S. BOMEDIANO Department of Education.
Earth History- Table of Contents
MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS
Presentation transcript:

Fractures, Faults, & Friction Lab # 5 Review Fractures, Faults, & Friction

Coulomb Failure Law

Byerlee’s Law 0.85 for low confining pressure, 0.6 for high confining pressure (>200 MPa)

Envelope of Frictional Sliding

Importance of Differential Sress As differential stress increases, the range of fractures with favorable orientations for reactivation increases

Sandbox Experiment normal faults on the left form at 60°, thrust faults on the right form at 30°

Anderson’s Theory of Faulting

Principal Stresses and Faulting Coulomb Failure criteria predicts that most rocks will fail at ~30° to sigma1

Balancing & Restoring Cross Sections Lab #7 Balancing & Restoring Cross Sections

Structure of the Lab Go through terminology and example Build a simple cross section (Problem 1) Restore a simple cross section (Problem 2) Start working on assignment, Problem 3

Cross Sections Deformed Cross Section: subsurface geology as it is now Restored Cross Section: what subsurface looked like before deformation Balanced Cross Section: deformed cross section capable of being restored

Fold and Thrust Belt result of crustal shortening    Older Younger Foreland Hinterland   • the area in front of the thrusts toward which the thrust sheet moved is the foreland • the region behind the thrusts is the hinterland • ramp is a fault that cuts across bedding, usually connecting two flats blind thrust  ramp flat

Assumptions Conservation of Area Consistency of Bed Length Plane Strain Break-Forward Sequencing Forward Ramping Faults Kink-Style Folds

Kink Folds cylindrical folds with angular hinges, assymetric

Kink Method Example • We first find the line L12 that bisects the angle between dips 1 and 2 • Extend the dips out to L12. When you cross the line, continue with the dip on the opposite side

Continue Plotting Axial Traces (Steven Dutch)

Completed Beds (Steven Dutch)

Fill in the Lithologic Units (Steven Dutch)

Restoring a Cross Section Identify the foreland & hinterland Identify the transport direction Choose a pin line Label each point where the trace of the axial plane of a fold crosses a contact - these will be your line segment end-points restore youngest fault first restore line segments evaluate your loose line

Bed Length Conservation • If you encounter a folded layer in the deformed cross section that does not intersect a fault, simply reproduce it as a horizontal line in the restored section. Bed Length Conservation

Restoring a Cross Section - Faults • Follow the fault in the direction opposite the Transport Direction until you hit the ramp. Draw a horizontal line segment at the top of the ramp with the same length as you measured above for the line segment. • follow the fault in the direction opposite the Transport Direction until you hit the ramp. Draw a horizontal line segment at the top of the ramp with the same length as you measured above for the line segment. • Faults should be reproduced as they are (without making lines horizontal) unless they show signs of being folded by younger stage faulting. This is part of why we restore youngest faults first!

Chevron Fold

Kink bands