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forces acting on the structure such as magnetic , inertial , gravitational , electrostatic , pressure , frictional , or viscous fluid flow forces(passive) can be caused byDeformation in micromechanical structures
External loadscausedeformation in structures
the manufacturing processleadsto the deformation of structures
falling stones which have loosened from lumps of ice(passive) caused byfossiled deformation structures ,
because the process uses heathas causeddeformation in some structures
Depletion of E2F1 or kinesins ( KIF2C , KIF18B , KIF20Aledto deformation of microtubule structures
due toPan - African Orogenycausedthe deformation of subsurface structures
about 37 ° C. Temperature gradients are avoidedto preventdeformation of the structures
The markedly reduced brain volumecausesdeformation of craniofacial structures
no explosion ,could causedeformation of the structures
from the low cycle fatigue of near - alpha titanium alloy Ti-6242Si Sudha Joseph | Ioannis Bantounas |resultingfrom the low cycle fatigue of near - alpha titanium alloy Ti-6242Si Sudha Joseph | Ioannis Bantounas |
from the migration of an upper Devonian aeolian dune | Journal of Sedimentary Research | GeoScienceWorld Journal of Sedimentary Research ( 1972 ) 42 ( 4resultingfrom the migration of an upper Devonian aeolian dune | Journal of Sedimentary Research | GeoScienceWorld Journal of Sedimentary Research ( 1972 ) 42 ( 4
from the migration of an upper Devonian aeolian dune | Journal of Sedimentary Research Skip to main content Deformation structures in siltstone resulting from the migration of an upper Devonian aeolian dune Brian G. Jones DOIresultingfrom the migration of an upper Devonian aeolian dune | Journal of Sedimentary Research Skip to main content Deformation structures in siltstone resulting from the migration of an upper Devonian aeolian dune Brian G. Jones DOI
from loss of support due to undercutting by lateral stream erosion at the base of a river bluffwould resultfrom loss of support due to undercutting by lateral stream erosion at the base of a river bluff
from three main deformation phasesresultfrom three main deformation phases
from the earthquakesresultingfrom the earthquakes
to significant riftingleadto significant rifting
the counteractive effect on flow field(passive) caused bythe counteractive effect on flow field