Fault trace
A fault trace describes the intersection of a geological fault with the Earth's surface, which leaves a visible disturbance on the surface, usually looking like a crack in the surface with jagged rock structures protruding outward. The term also applies to a line plotted on a geological map to represent a fault. These fractures tend to occur when a slip surface expands from a fault core, especially during an earthquake. This tends to occur with fault displacement, in which surfaces on both sides of a fault, known as fault blocks, separate horizontally or vertically.[1]
See also
References
- Torabi, Anita; Berg, Silje Støren (2011-08-01). "Scaling of fault attributes: A review". Marine and Petroleum Geology. 28 (8): 1444–1460. doi:10.1016/j.marpetgeo.2011.04.003. ISSN 0264-8172.
- Balance, P. F. (2009-04-08). Sedimentation in Oblique-slip Mobile Zones. John Wiley & Sons. ISBN 978-1-4443-0374-2.
- Bouchon, Michel (1980). "The motion of the ground during an earthquake: 2. The case of a dip slip fault". Journal of Geophysical Research: Solid Earth. 85 (B1): 367–375. doi:10.1029/JB085iB01p00367. ISSN 2156-2202.
- Katz, Yoram; Weinberger, Ram; Aydin, Atilla (2004-03-01). "Geometry and kinematic evolution of Riedel shear structures, Capitol Reef National Park, Utah". Journal of Structural Geology. 26 (3): 491–501. doi:10.1016/j.jsg.2003.08.003. ISSN 0191-8141.
- Treiman, Allan H. (March 2008). "Ancient groundwater flow in the Valles Marineris on Mars inferred from fault trace ridges". Nature Geoscience. 1 (3): 181–183. doi:10.1038/ngeo131. ISSN 1752-0908.
- Philip, G. (2007-11-01). "Remote sensing data analysis for mapping active faults in the northwestern part of Kangra Valley, NW Himalaya, India". International Journal of Remote Sensing. 28 (21): 4745–4761. doi:10.1080/01431160701264243. ISSN 0143-1161.
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