lecture11
Table of Contents
- Deformation of Rocks
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- Why study rock deformation?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.1 What do deformed rocks look like?
- 11.2 How are resources related to geologic structures?
- 11.2 How are resources related to geologic structures?
- 11.2 How are resources related to geologic structures?
- 11.2 How are resources related to geologic structures?
- 11.3 Why do rocks deform?
- 11.3 Why do rocks deform?
- 11.3 Why do rocks deform?
- 11.3 Why do rocks deform?
- 11.3 Why do rocks deform?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.4 How do we know ... why some rocks break and others flow?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.5 How do geologic structures relate to stress, strain, and strength?
- 11.6 How does strength vary in the lithosphere?
- 11.6 How does strength vary in the lithosphere?
- 11.6 How does strength vary in the lithosphere?
- 11.7 How do earthquakes relate to rock deformation?
- 11.7 How do earthquakes relate to rock deformation?
- 11.7 How do earthquakes relate to rock deformation?
- 11.7 How do earthquakes relate to rock deformation?
- Elastic Rebound
- 11.7 How do earthquakes relate to rock deformation?
- 11.7 How do earthquakes relate to rock deformation?
- 11.7 How do earthquakes relate to rock deformation?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.8 How are earthquakes measured?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
- 11.9 Why are earthquakes destructive?
Text and Images from Slide
- At different combinations of stress and strain rocks exhibit elastic, brittle, or plastic deformation.
- Increasing confining pressure increases rock strength and leads to plastic flow rather than brittle fracture.
- Increasing temperature decreases rock strength and enhances plastic flow.
- Wet rocks are weaker than dry rocks at the same temperature and confining pressure.
11.4 How do we know ... why some rocks break and others flow?