- horizontal,
parallel to the
fault trace; dip-slip,
offset is
predominantly vertical and/or
perpendicular to the
fault trace; or
oblique-slip,
combining strike-slip...
-
Faults can be
classified into four
types based on the kind of
motion between the
separated rock m****es: normal, reverse, strike-slip, and
oblique. While...
-
continental transform faults,
zones of
oblique collision and the
deforming foreland of
zones of
continental collision. When strike-slip
fault zones develop,...
- A
transform fault or
transform boundary, is a
fault along a
plate boundary where the
motion is
predominantly horizontal. It ends
abruptly where it connects...
- Sea plate. This left-lateral strike-slip
fault extends NW-SE (N30 – 40 W)
accommodating the
lateral oblique motion of the
subducting Philippine Sea plate...
-
known as the San Juan
fault to its
current easterly orientation. This also
initiated the
oblique left-lateral
Devils Mountain fault,
including the section...
- seismically-active
faults in the
North Island of New
Zealand that
carry much of the
dextral (right lateral) strike-slip
component of the
oblique convergence...
-
including forearc slivers and
strike slip
fault systems that are sub-parallel to
ocean trenches. In addition,
oblique subduction is ****ociated with the closure...
-
Santa Ana River, one of the
upper branches of the
fault. This
fault is a
reverse right-
oblique fault. It is most
known for the Whittier, Brea-Olinda, Sansinena...
- The
Garrapatas Fault (Zone) (Spanish: (Zona de) Falla(s) de Garrapatas) is an
inactive dextral oblique thrust fault in the
departments of Chocó and Valle...