![]() ![]() Strike-slip faults are often associated with large displacements. Transform faults are one of the three basic elements of plate kinematics and those that cut continental crust are among the most notable and most notorious geological features on the present earth. The image shows a 140-km-wide region at the eastern end of Agenor Linea, a 1500-km-long prominent bright band in Europas southern hemisphere that has undergone up to 20 km of right-lateral offset ( Prockter et al., 2000 ). A strike-slip fault is one that shows horizontal slip parallel to the strike of a vertical or subvertical fault plane. Faults are classified using the angle of the fault with respect to the surface (known as the dip) and the direction of slip along the fault. INTRODUCTION Plate tectonics involves major strike-slip faulting. ![]() The Ridge Basin is a type of fault-bend basin developed in front of a releasing bend on the San Gabriel Fault, along which the upper crust stretched and subsided to form a space in which sediments could be accommodated. ![]() Trending Questions What is the collection of ancient stars found in the center of the local group called? What is the flickering star in the eastern sky tonight? What is cyclic universe theory? How will the fusion rate of a two solar mass star compare to the fusion rate of a four solar mass star? According to the big bang theory the universe began as a? Why will light from two closely spaced stars not produce a steady interference pattern at the earth's surface? Which philosopher believed the universe was an explosion? How is resolution affected by the size of a telescopes mirror or lens? Stars can be classified into groups based on their? What always contains ice comets Asteroids or meteors? What three things does the sun provide for the earth? What are the parts of the eclipse? How often does a one-kilometer object hit Earth? Is Ringo star dead? A star has apparent magnitude 10.0 and absolute magnitude 2. Strike-slip faults, which are among the straightest and longest geologic features on Earth, are often identified by their geomorphic expression, including hallmarks such as offset rivers, shutter ridges, sag ponds, and linear, strike-parallel valleys e.g., Wallace, 1949 Hill and Dibblee, 1953. In contrast to the two ridge-like fault examples, the strike-slip fault in Fig. The San Gabriel Fault is a listric, ESE-dipping, oblique-slip fault rather than a subvertical, strike-slip fault. ![]()
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