PGE 383 (16367) Spring 1997
ABSTRACT: This course will treat natural fractures in rock (veins, dikes, joints and faults) from a predictive, mechanical perspective. We will cover the basics of engineering fracture mechanics and how it can be applied to geologic and reservoir fracture problems. Fracture opening and slip distributions, spacing, propagation paths, stress drops, and near-tip processes will be analyzed, using geologic examples as constraints for theoretical models. Problems will be considered at the crustal, reservoir and outcrop scale. In addition, we will discuss models for in situ stress magnitudes and the role of pore pressure in rock fracture. Students will be introduced to 2d and 3d elastic fracture codes for predicting stress, strain and displacements induced by fractures. Although the course will emphasize the mechanical aspects of fracture, the impact of fractures on subsurface permeability will be an integral part of our discussion.
Jon Olson
Dept. of Petroleum and Geosystems Engineering
Office: CPE 5.168B
phone: 471-7375
e-mail: jolson@pe.utexas.edu
Office hours: MWF 1-2.
MWF 11am, 3 credits, Rm. CPE 2.206.
Mid-term Exam, 30%
Problem sets, 30%
Final Project, 30%
Class participation, 10%
The University of Texas at Austin provides upon request appropriate adjustments for qualified students with disabilities. For more information, contact the Office of the Dean of Students at 471-6259, 471-4241 TDD or the College of Engineering Director of Students with Disabilities at 471-4382.
Scholastic dishonesty will not be tolerated and incidents of dishonesty will be reported.
Introduction, discussion of syllabus
Fracture morphology
Introduction to Fracture Mechanics
Basic Jointing Theory
Natural hydraulic fracturing
Fracture networks
Deformation field around faults
Reservoir engineering
Fracture Mechanics of Rock, 1987, Barry Kean Atkinson, ed., Academic Press, 534 p.
Additional References:
Fracture of Brittle Solids, 1975, B. R. Lawn and T. R.
Wilshaw, Cambridge University Press, 204 p.
Surface morphology on cross-fold joints of the Appalachian Plateau, New York and Pennsylvania, Bahat and Engelder, Tectonophysics 104, p. 299-313, 1984.
IGC Fieldtrip Y385: Physical and hydrologic-flow properties of fractures, Barton and Hsieh, 28th Int. Geol. Cong., Fieldtrip Guidebook T385, 1989.
Fluid flow along potentially active faults in crystalline rock, Barton, Zoback and Moos, Geology 23(8), p. 683-686, 1995.
Field relations between dikes and joints: emplacement processes and paleostress analysis, Delaney, Pollard, Ziony, and McKee, JGR 91(B5), p. 4920-4938, 1986.
Orthogonal fracture systems at the limits of thrusting: an example from southwestern Wales, Dunne and North, JSG 12(2), p. 207-215, 1990.
Using joint interactions to estimate paleostress ratios, Dyer, JSG 10(7), p. 685-699, 1988.
Natural hydraulic fracturing , Engelder and Lacazette, Proc. of Int. Symp. on Rock Joints, Loen, Norway, June 4-6, 1990, p. 35-43.
The origin and spacing of cross joints: examples from the Monterey Formation, Santa Barbara Coastline, California, Gross, JSG 15(6), p. 737-751, 1993.
Classification of structures on joint surfaces, Hodgson, Amer J. Sci. 259, p. 493-502, 1961.
Regional study of jointing in Comb Ridge Navajo Mountain area, Arizona and Utah, Hodgson, AAPG 45(1), p. 79-116, 1961.
The fracture process zone in granite: Evidence and effect, Labuz, Shah, Dowding, Int. J. Rock Mech. Min. Sci. & Geomech Abstr 24(4), p. 235-246, 1987.
Differences in fracture characteristics and related production: Mesaverde Formation, Northwestern Colorado, Lorenz and Finley, SPE Form. Eval, p. 11-16, 1989.
Regional fractures II: Fracturing of Mesaverde reservoirs in the Piceance Basin, Colorado, Lorenz and Finley, AAPG 75(11), p. 1738-1757, 1991.
Regional fractures I: A mechanism for the formation of regional fractures at depth in flat-lying reservoirs, Lorenz, Teufel and Warpinski, AAPG 75(11), p. 1714-1737, 1991.
Small-scale fracture density in Asmari Formation of Southwest Iran and its relation to bed thickness and structural setting, McQuillan, AAPG 57(12), p. 2367-2385, 1973.
Fracture density in the deep subsurface: techniques with application to Point Arguello Oil Field, Narr, AAPG 75(8), p. 1300-1323, 1991.
Joint spacing in sedimentary rocks, Narr and Suppe, JSG 13, p. 1037-1048, 1991.
Joint pattern development: effects of subcritical crack growth and mechanical crack interaction, Olson, JGR 98(B7), p. 12251-12265, 1993.
The initiation and growth of en echelon veins, Olson and Pollard, JSG 13(5), p. 595-608, 1991.
Inferring paleostresses from natural fracture patterns: a new method, Olson and Pollard, Geology 17, p. 345-348, 1989.
Progress in understanding jointing over the past century, Pollard and Aydin, GSA Bull 100(8), p. 1181-1204, 1988.
Formation and interpretation of dilatant echelon cracks, Pollard, Segall and Delaney, GSA Bull. 93, p. 1291-1303, 1982.
Joint development in perturbed stress fields near faults, Rawnsley, Rives, Petit, Nencher and Lumsden, JSG 14(8/9), p. 939-951, 1992.
Analogue simulation of natural orthogonal joint set formation in brittle varnish, Rives, Rawnsley and Petit, JSG 16(3), p. 419-429, 1994.
Joint spacing: analogue and numerical simulations, Rives, Razack, Petit and Rawnsley, JSG 14(8/9), p. 925-937, 1992.
Role of fluid pressure in jointing, Secor, Amer J. Sci 263, p. 633-646, 1965.
Rate-dependent extensional deformation resulting from crack growth in rock, Segall, JGR 89(B6), p. 4185-4195, 1984.
Formation and growth of extensional fracture sets, Segall, GSA Bull 95, p. 454-462, 1984.
Joint formation in granitic rock of the Sierra Nevada, Segall and Pollard, GSA Bull. 94, p. 563-575, 1983.
Nucleation and growth of strike slip faults in granite, Segall and Pollard , JGR 88(B1), p. 555-568, 1983.