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GEOL 306. Structural Geology and Field Methods (5) I
Two lectures and three hours of laboratory and six weekends in the field.
Prerequisites: Geological Sciences 300, 324; algebra, trigonometry and at least high school physics. Highly recommended: First semester college physics.
Integrates structural and introductory field geology. Principles, causes, and mechanisms of rock deformation combined with field study. Graphical, computer, and analytical techniques for working with folds and faults are applied in the field. Field observations are presented in geologic maps, cross sections, and reports.

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Quartz: SiO
2
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Structural Geology is the branch of the geological sciences that deals with the earth’s crust and mantle from a mechanical perspective. We know a great deal about the history of our planet based on careful field observations of deformed rocks and the large and small-scale structures that have resulted from tectonic events. Structural Geology also encompasses targeted experimental investigations into rock deformation, and draws from the allied fields of geophysics, material science and mechanical engineering. This course seeks to build on your introductory field experiences and preparatory geology, mathematics, and physics courses. We will first focus on descriptive structure and the classification, measurement, and mapping of key structural features. The course moves on to examine stress and strain in more detail along with smaller-scale structures observable and mappable in field settings. The final section of this course examines the microstructural basis of solid-state deformation in earth materials, exploring the quantitative treatment and mineral-grain scale mechanical processes which make possible all deformation events. The overall goal is to provide an integrated map-to-microscope perspective on movement in the earth’s crust and mantle, leading to a fuller understanding of deformation events and the stresses in the earth which cause them.

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Instructor
Web Site
Syllabus
Dr. Gary Girty
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Stereonet - Wulff equal angle
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Stereonet - Schmidt equal area
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