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slip fault वाक्य

"slip fault" हिंदी मेंslip fault in a sentence
उदाहरण वाक्यमोबाइल
  • The Itremo sheet was faults, and strike-slip faults.
  • A special class of strike-slip faults is the transform fault, where such faults form a plate boundary.
  • End member structures include pure strike-slip faults and purely extensional ( " normal " ) dip-slip faults.
  • End member structures include pure strike-slip faults and purely extensional ( " normal " ) dip-slip faults.
  • Focal mechanism solutions strike NE and frequently demonstrate normal dip-slip faults, although left-lateral motion is also observed.
  • Geologists call both faults right-handed strike-slip faults.
  • Neither Durer appears to be slightly offset on the north side by a small normal or strike-slip fault.
  • The Turkey earthquake occurred along a strike-slip fault, similar to the San Andreas fault that runs beneath California.
  • The structure of the Buck Creek basin is rift-related, controlled by a series of northwest-southwest trending strike-slip faults.
  • A fault which has a component of dip-slip and a component of strike-slip is termed an " oblique-slip fault ".
  • The alteration of the Pacific Plate  s motion caused a left-lateral strike-slip fault to form at the Pacific-Antarctic Boundary.
  • They also form where two segments of a strike-slip fault overlap, and the relay zone between the segments experiences transtension.
  • Both are strike slip faults nearly 1, 000 miles long, storing tremendous energy generated at the confluence of tectonic plates.
  • The "'geology of Chile "'is a result of the Andean and preceding Nazca and Antarctic Plates or shallow strike-slip faults.
  • It was during the Miocene, that these strata were translated to their present position by movement along detachment and strike-slip faults.
  • It has the characteristics of a strike-slip fault, in which one huge chunk of land slides by another one, she said.
  • During the Oligocene to Miocene, many of the basement faults were reactivated by the strike-slip faults during the Late Cretaceous inversion.
  • This suggests that the OWL was once a strike-slip fault, possibly a continental margin, along which terranes moved from the southeast.
  • Farther north and east, the ANS was affected by the formation of the great NW-SE trending Najd system of strike-slip faults.
  • Four of the region's known strike-slip faults and one additional newly discovered normal fault all broke the surface during the earthquake.
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