Riedel Shears
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The Riedel shears (also called R shears) are the small right-lateral faults which are gently inclined to the strike of the main fault. Their presence suggests ... RiedelShears Thisphotoislookingstraightdownontoafaultzone.TheRiedelshears (alsocalledRshears)arethesmallright-lateralfaultswhicharegently inclinedtothestrikeofthemainfault.Theirpresencesuggestsoverall right-lateralmotiononthezone. Anotherexample... RiedelshearimmediatelybelowBadwaterTurtlebackfault,DeathValley, CA.Rshearsuggestsoveralltop-to-rightmotionwhichaccordswithevidence elsewherealongthefault.Notereddishgougezonealongfaultsurface. BacktoSlipdirectionsonfaults.
延伸文章資訊
- 1Typical Riedel shear structures of the coseismic surface ...
An ideal Riedel shear zone generally consists of six principal elements (Fig. 6): Riedel (R) and ...
- 2Riedel Shears
The Riedel shears (also called R shears) are the small right-lateral faults which are gently incl...
- 3(PDF) Riedel shear: a mechanism for ... - ResearchGate
Cleavage, as Riedel (R) shears nucleates obliquely to planar anisotropy of foliated rocks and at ...
- 4Conjugate Riedel deformation band shear zones
The antithetic R'-shears depart by H758 from the Riedel shear zones of which they are a part, and...
- 5Riedel shears Archives - Geological Digressions
Riedel shears: Parallel arrays of faults that form during the early stages of strike-slip formati...
