'Dip slip faults' diaporamas de présentation

CHAPTER 8

CHAPTER 8. FAULTS AND FAULTING Dr. Masdouq Al-Taj. FAULTS. A fault is any surface or zone in the Earth across which measurable slip (shear displacement) develops. Faults are fractures on which slip develops primarily by brittle deformation processes.

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Ch. 17 Crustal Deformation and Mountain Building

Ch. 17 Crustal Deformation and Mountain Building. Chapter 17 Opening Figure. Rock Deformation. Rock deformation refers to changes in the shape, volume, or orientation of a rock due to changes in temperature and pressure over time. Rock Deformation due to Stress.

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Module-8

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Faults and Earthquakes

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Faults and Earthquakes

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Dip-slip faults

Dip-slip faults. Goal : To interpret dip-slip faults on seismic sections and to build on your interpretations to understand normal-fault and thrust-fault systems. Part-I : Normal-fault systems. Seismic-reflection profile of a large normal fault. Seismic-reflection profiles.

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Structural Geology

Structural Geology . Deformation of rocks produces: folds, joints, faults. Monocline - southeastern Utah. Northeastern California - note tilted layers. http://faculty.uaeu.ac.ae/~afarrag/physical%20geology/GEODE1.jpg. Wasatch Front NE of Salt Lake City, UT. Types of Stresses.

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