strike slip वाक्य
उदाहरण वाक्य
मोबाइल
- Transtensional settings are believed to generate greater surface subsidence than pure-strike slip alone.
- The San Andreas and North Anatolian faults are textbook examples of right lateral strike slip faults.
- Thrust faults are generated by the highest, strike slip by intermediate, and normal faults by the lowest stress levels.
- Strike slip duplexes occur at the step over regions of faults, forming a lens shaped near parallel arrays of horses.
- Both are strike slip faults nearly 1, 000 miles long, storing tremendous energy generated at the confluence of tectonic plates.
- Because the basin lies on the boundary of the Transverse and Peninsular Ranges, this basin experiences both compressional and strike slip tectonics.
- As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress.
- A regional sandbox models have shown that the geometry and evolution of pull-apart basins varies greatly in pure-strike slip situations versus transtensional settings.
- The numerous strike slip faults in the area could be involved too, whereas subduction of the Tarim Basin beneath the Kunlun is unlikely.
- It rises approximately above the mean level of the northeastern Pacific Ocean and lies directly along the southern expression of the left laterial, strike slip Nootka Fault.
- On a " strike slip " fault such as the San Andreas, one side of the fault releases seismic strain by abruptly jolting sideways past the other.
- The dominating feature of the fracture zone is the 150 km long Blanco Ridge, which is a high-angle right-lateral strike slip fault with some component of dip-slip faulting.
- On a larger scale, a zone between offset strike slip faults may have minor " en echelon " fault strands that accommodate the shearing motion induced in the region.
- The syntaxis on either side of the Himalaya are dominated by a strike slip fault zone, instead of a compressional thrust faulting, as in the rest of the orogen.
- Faulting shifts the ground in a vertical motion through reverse, normal or oblique strike slip faulting processes, this displaces the water above causing a tsunami ( Figure 1 ).
- The partitioning of strain occurs through the development of a strike slip or shear zone ( shown with red arrows ) across the actively deforming region ( brown ).
- A viable method proposed to make room from ascending magma is a zone of lateral extension which can be found at mid ocean ridges, strike slip faults and dialational jogs.
- The formation is bounded on its edges by a series of high-angle strike slip faults, which have contained the Klondike Mountain Formation in a series of graben structures, such as the Republic Graben.
- The "'Septentrional-Orient fault zone "'( SOFZ ) is a system of coaxial left lateral-moving strike slip faults which runs along the northern side of the island of Hispaniola where Haiti and the Dominican Republic are located.
- We do not mean to suggest that an earthquake with simultaneous ruptures of thrust and strike slip is imminent . . . . Rather, the similarities are too great for the possibility of such an event to be ignored.
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