-
listric faults. Cross-section
diagram of a
listric fault Cross-section
diagram of
multiple listric faults in a
cliff wall The
fault panes of
listric faults...
-
Extensional environments like the
Basin and
Range are
characterized by
listric normal faulting, or
faults that
level out with depth.
Opposing normal faults...
-
province is 500 m (1,640 ft) deep, but it is
unknown whether it is a
shallow listric fault or
penetrates deeply. All
historical eruptions occurred at either...
-
structure developed within the
downthrown block (hanging wall) of
large listric normal faults. Such
faults are
typically regional in
nature and develop...
-
Hibernia structure is
bounded on the west by the north-northeast
trending listric Murre Fault and on the
northeast by the
Nautilus Fault.: 36 and 42 Late...
-
Extensional environments like the
Basin and
Range are
characterized by
listric normal faulting, or
faults that
level out with depth.
Opposing normal faults...
-
rapid (catastrophic) subsidence.
Growth faults are also
sometimes called "
listric faults",
implying that the
fault is a concave-upward
surface that transforms...
-
extension that can
accommodate for the
extensive down fall of the grabens.
Listric faults produce the
correct model for this
sufficient crustal extension...
- bend
folds occur in both
extensional and
thrust faulting. In extension,
listric faults form
rollover anticlines in
their hanging walls. In thrusting, ramp...
-
Schematic structural profile of the
Niger Delta,
which is
characterized by
listric extension faults,gentle
folds thrusts, and diapirs.
Image modified from...
