- In geology,
aseismic creep or
fault creep is
measurable surface displacement along a
fault in the
absence of
notable earthquakes.
Aseismic creep may also...
- is the
cause of most earthquakes.
Faults may also
displace slowly, by
aseismic creep. A
fault plane is the
plane that
represents the
fracture surface...
-
fault plane. The
sides of a
fault move past each
other smoothly and
aseismically only if
there are no
irregularities or
asperities along the
fault surface...
- The ocean-floor of the
Indian Ocean is
divided by
spreading ridges and
crisscrossed by
aseismic structures...
-
deformation front.
Further down-dip, a
transition from
fully locked to
aseismic sliding occurs.
Unlike most
subduction zones worldwide, no
oceanic trench...
- rest of the
central section of the
fault exhibits a
phenomenon called aseismic creep,
where the
fault slips continuously without causing earthquakes....
-
reports of
luminous phenomena (UFO Reports) – Is the
strain field an
aseismically propagating hydrological pulse?. Derr, J.S. (1993).
Perceptual and Motor...
- sei-
shake Gr**** σείειν (seíein), σεισμός (seismós), σεῖστρον (seîstron)
aseismic, microseism, microseismic, paleoseismology, seism, seismic, seismogram...
- The
Nazca Plate or
Nasca Plate,
named after the
Nazca region of
southern Peru, is an
oceanic tectonic plate in the
eastern Pacific Ocean basin off the...
- side that have
shifted more than five feet
relative to one
another due to
aseismic creep since the
bridge was
constructed in 1936.
Google satellite images...
