-
Given a
family of curves, ****umed to be differentiable, an
isocline for that
family is
formed by the set of
points at
which some
member of the
family attains...
- well-developed
axial planar cleavage.
Isoclinal folds with east-striking
axial planes become overturned to the north. Such
isoclinal folding is
interpreted to have...
-
geological environment.
Deposits are
typically found in the "hinge" of
isoclinal folds.
There are many
accounts of the
discovery of tanzanite, but only...
-
folds from 70° to 30°, and
tight folds from 30° to 0°. Isoclines, or
isoclinal folds, have an
interlimb angle of
between 10° and zero, with essentially...
- long
scale crustal shortening during the
Mazatzal orogeny which formed isoclinal folds and
shear zones.
North Mountain and Shaw Butte,
which are composed...
-
deformation have been identified, the most
important being large scale isoclinal folding with axes
aligned north-west. The T-zone is
deformed and is interpreted...
-
surrounding migmatite-gneiss complexes,
these low-grade
metamorphic rocks have
isoclinal folding and
steeply dipping foliation. They have
faulted and
sheared boundaries...
- Lift-off
detachment folds are
characterized by
isoclinal folding in all units, with a
tight isoclinal folded weak unit in the
anticline and
parallel geometries...
-
strata of the
Nastapoka Group become highly faulted and tightly,
often isoclinally, folded.
These strata unconformably overlie Archean strata of the Superior...
-
Isoclinally folded Bündner
schists with
alternating green (chlorite rich) and
white (dolomite rich) layers. Location:
Adula nappe,
Lukmanier p**** (Switzerland)...
