Describe the type of faulting you would expect to see at each of the following settings, including a sketch of the fault, and a fault plane solution (i.e. beachball) indicating where you might expect compressional and dilational first motions: a) a transform fault b) a fast-spreading mid-ocean ridge c) a continental collision zone What kind of focal mechanism might be associated with an underground mine collapse?

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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**Text from Educational Resource:**

**Faulting Types and Focal Mechanisms**

1. **Transform Fault**

   - Transform faults are where two tectonic plates slide past one another. The fault is typically vertical, and the motion is horizontal.
   - Fault Plane Solution: Usually depicted as a "beachball" diagram showing a combination of compressional and extensional forces. Compressional first motions can be expected on one side of the fault while dilational (extensional) first motions occur on the other.
   - Sketch: Illustrate a vertical fault line with opposite arrows indicating horizontal movement of the plates.

2. **Fast-Spreading Mid-Ocean Ridge**

   - At mid-ocean ridges, tectonic plates are pulling apart, creating new oceanic crust. This setting often features normal faults due to tensional forces.
   - Fault Plane Solution: Beachball diagrams commonly show predominantly extensional first motions, indicating crustal separation.
   - Sketch: Show diverging lines with arrows pointing away from each other, representing the spreading plates.

3. **Continental Collision Zone**

   - These zones occur where two continental plates collide, resulting in compressional forces and thrust faulting.
   - Fault Plane Solution: Beachball diagrams reveal compressional first motions, typical of thrust or reverse faults.
   - Sketch: Illustrate converging lines with arrows pointing towards each other to represent the collision forces.

**Focal Mechanism for Underground Mine Collapse**

- An underground mine collapse often results in a localized inward motion, predominantly involving subsidence or cave-in events.
- The focal mechanism may display dilational first motions in the surrounding areas due to material displacement toward the collapse point.
Transcribed Image Text:**Text from Educational Resource:** **Faulting Types and Focal Mechanisms** 1. **Transform Fault** - Transform faults are where two tectonic plates slide past one another. The fault is typically vertical, and the motion is horizontal. - Fault Plane Solution: Usually depicted as a "beachball" diagram showing a combination of compressional and extensional forces. Compressional first motions can be expected on one side of the fault while dilational (extensional) first motions occur on the other. - Sketch: Illustrate a vertical fault line with opposite arrows indicating horizontal movement of the plates. 2. **Fast-Spreading Mid-Ocean Ridge** - At mid-ocean ridges, tectonic plates are pulling apart, creating new oceanic crust. This setting often features normal faults due to tensional forces. - Fault Plane Solution: Beachball diagrams commonly show predominantly extensional first motions, indicating crustal separation. - Sketch: Show diverging lines with arrows pointing away from each other, representing the spreading plates. 3. **Continental Collision Zone** - These zones occur where two continental plates collide, resulting in compressional forces and thrust faulting. - Fault Plane Solution: Beachball diagrams reveal compressional first motions, typical of thrust or reverse faults. - Sketch: Illustrate converging lines with arrows pointing towards each other to represent the collision forces. **Focal Mechanism for Underground Mine Collapse** - An underground mine collapse often results in a localized inward motion, predominantly involving subsidence or cave-in events. - The focal mechanism may display dilational first motions in the surrounding areas due to material displacement toward the collapse point.
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