Book contents
- Frontmatter
- Contents
- How to use this book
- Preface
- Acknowledgments
- List of symbols
- 1 Structural geology and structural analysis
- 2 Deformation
- 3 Strain in rocks
- 4 Stress
- 5 Stress in the lithosphere
- 6 Rheology
- 7 Fracture and brittle deformation
- 8 Faults
- 9 Kinematics and paleostress in the brittle regime
- 10 Deformation at the microscale
- 11 Folds and folding
- 12 Foliation and cleavage
- 13 Lineations
- 14 Boudinage
- 15 Shear zones and mylonites
- 16 Contractional regimes
- 17 Extensional regimes
- 18 Strike-slip, transpression and transtension
- 19 Salt tectonics
- 20 Balancing and restoration
- 21 A glimpse of a larger picture
- Appendix A More about the deformation matrix
- Appendix B Stereographic projection
- Glossary
- References
- Cover and chapter image captions
- Index
Preface
- Frontmatter
- Contents
- How to use this book
- Preface
- Acknowledgments
- List of symbols
- 1 Structural geology and structural analysis
- 2 Deformation
- 3 Strain in rocks
- 4 Stress
- 5 Stress in the lithosphere
- 6 Rheology
- 7 Fracture and brittle deformation
- 8 Faults
- 9 Kinematics and paleostress in the brittle regime
- 10 Deformation at the microscale
- 11 Folds and folding
- 12 Foliation and cleavage
- 13 Lineations
- 14 Boudinage
- 15 Shear zones and mylonites
- 16 Contractional regimes
- 17 Extensional regimes
- 18 Strike-slip, transpression and transtension
- 19 Salt tectonics
- 20 Balancing and restoration
- 21 A glimpse of a larger picture
- Appendix A More about the deformation matrix
- Appendix B Stereographic projection
- Glossary
- References
- Cover and chapter image captions
- Index
Summary
This textbook is written to introduce undergraduate students, and others with a general geologic background, to basic principles, aspects and methods of structural geology. It is mainly concerned with the structural geology of the crust, although the processes and structures described are relevant also for deformation that occurs at deeper levels within our planet. Further, remote data from Mars and other planets indicate that many aspects of terrestrial structural geology are relevant also beyond our own planet.
The field of structural geology is very broad, and the content of this book presents a selection of important subjects within this field. Making the selection has not been easy, knowing that lecturers tend to prefer their own favorite aspects of, and approaches to, structural geology, or make selections according to their local departmental course curriculum. Existing textbooks in structural geology tend to emphasize the ductile or plastic deformation that occurs in the middle and lower crust. In this book I have tried to treat the frictional regime in the upper crust more extensively so that it better balances that of the deeper parts of the crust, which makes some chapters particularly relevant to courses where petroleum geology and brittle deformation in general are emphasized.
Obtaining this balance was one of several motivating factors for writing this book, and is perhaps related to my mixed petroleum geology and hard-rock structural geology experience.
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- Chapter
- Information
- Structural Geology , pp. xiPublisher: Cambridge University PressPrint publication year: 2010