Structural Geology
Geological Sciences 351 - 2000
Monday, Wednesday, Friday, 11 am - 12 noon, Room 2520 CCL (Lectures)
Monday, Wednesday, 2 pm - 5 pm, Room 3526 CCL (Laboratory)
Josep M. Pares,
jmpares@umich.edu,
4506 C.C. Little Building, 734-615-0472.
Graduate Student Instructor: Arlo Weil, C.C. 4534 C.C. Little Building, 734-763-2149.
GS351. Structural Geology.
G.S. 117 or 119 or the equivalent; or permission of instructor. (4). (Excl).
(BS). The description and analysis of geological structures in the Earth's
crust and an introduction to global tectonics. Three lectures and one laboratory
session weekly. The following topics are covered: the description of geological
structures; the kinematics and dynamics of folding and faulting; stress,
strain, deformation and rheology; introduction to dislocation theory; micro-structural
analysis; principles of plate tectonics; selected orogenic systems of the
world. This is a core course for concentrators, but is open to all who
want to have a basic knowledge of geology. Evaluation is based on graded
lab assignments, a lab test, and three exams.
Textbooks: Earth
Structure - An Introduction to Structural Geology and Tectonics, 1997,
by B.A. van der Pluijm and S. Marshak (lectures) and Basic Methods of Structural
Geology by S. Marshak and G. Mitra (labs).
Part I: Stress and Strain (January 5 - January 21):
Introduction and primary structures
Part II: Brittle Structures and Deformation Processes (January 24 - February 7):
Exam I (20%): February 11
Part III: Ductile Structures and Deformation processes (February 14 - March 15):
Part IV: Tectonics and Regional Deformation (March 17 - March 29):
Exam II (20%): March 31
Part V: Regional Geology (April 3 - April 12):
Precambrian Belts of North America
| Date |
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| W | 5-Jan | Introduction, Primary Structures |
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| F | 7-Jan | Forces and Stress |
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| M | 10-Jan | Forces and Stress |
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| W | 12-Jan | Deformation and Strain |
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| F | 14-Jan | Deformation and Strain |
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| M | 17-Jan | No Class – Martin Luther King Day |
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| W | 19-Jan | Rheology |
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| F | 21-Jan | Rheology |
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| M | 24-Jan | Brittle Deformation |
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| W | 26-Jan | Brittle Deformation |
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| F | 28-Jan | Brittle Deformation |
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| M | 31-Jan | Joints and Veins |
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| W | 2-Feb | Joints and Veins |
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| F | 4-Feb | Faulting |
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| M | 7-Feb | Faulting |
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| W | 9-Feb | Recitation |
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| F | 11-Feb | Exam I | ||
| M | 14-Feb | Ductile Deformation |
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| W | 16-Feb | Ductile Deformation |
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| F | 18-Feb | Ductile Deformation |
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| M | 21-Feb | Ductile Deformation |
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| W | 23-Feb | Folding |
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| F | 25-Feb | Folding |
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| M | 6-Mar | Folding |
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| W | 8-Mar | Foliations and Lineations |
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| F | 10-Mar | Foliations and Lineations |
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| M | 13-Mar | Shear Zones |
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| W | 15-Mar | Shear Zones |
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| F | 17-Mar | Thrusting |
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| M | 20-Mar | Strike-Slip Tectonics |
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| W | 22-Mar | Extensional Tectonics |
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| F | 24-Mar | Structural Geology and Plate Tectonics |
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| M | 27-Mar | Structural Geology and Plate Tectonics |
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| W | 29-Mar | Recitation |
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| F | 31-Mar | Exam II | ||
| M | 3-Apr | Regional Geology |
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| W | 5-Apr | Regional Geology |
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| F | 7-Apr | Regional Geology | ||
| M | 10-Apr | Regional Geology |
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| W | 12-Apr | Regional Geology |
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| F | 14-Apr | Recitation | ||
| M | 17-Apr |
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||
| F | 21-Apr | Exam III |
|
by Ben A. van der Pluijm and Stephen Marshak. WCB/McGraw-Hill, 495 p., 1997. ISBN: 0697172341. Check the Web for pricing, which may vary significantly (e.g., BigWords.com) Click to go to EarthStructure's Corrections page. |
Homework
The computer program
“stressmohr”
illustrates the use of stress calculations for two-dimensional systems.
The program consists of five displays. In each display you can vary the
physical situation and immediately see the effects in the graphical displays.
The first display illustrates the relation between forces and stresses
acting on a rectangular solid. In the second display, you explore the stress
on a plane as you vary the orientation of the plane and the state of stress
in the system. We illustrate the calculation of the stress on the plane
in terms of a simple matrix multiplication in the third display. You can
also observe the simple geometry of the envelope of the stresses that are
produced as the angle of the plane is varied. The fourth display shows
the behavior of the normal and shear components of the stress on the plane.
When the normal component is plotted along x and the shear component along
y, the envelope will be a circle: called a Mohr circle. This beautiful
result lets you visualize the range of possible stresses on the plane.
Finally in the last display, you can explore the conditions which lead
to the fracture of a sample: you can vary the stresses until the stresses
are just strong enough to cause fracture by watching the changes in size
and location of the Mohr circle.
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Instructional
Supplements (links to EarthStructure)
Geological
Sciences at the University of Michigan
Tectonophysics
at the University of Michigan
Last Revised: January 2000
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