- with
superimposed smaller folds.
Synclines are
typically a
downward fold (
synform),
termed a
synformal syncline (i.e. a trough), but
synclines that point...
- upwards,
creating "antiforms", or
where it
buckles downwards,
creating "
synforms". If the tops of the rock
units within the
folds remain pointing upwards...
-
Basin '
synform' that
forms the
Chilterns (and
further west, the
Berkshire Downs), and the
chalk and
later deposits that have
filled both
synforms. The oldest...
-
Victor Grignard (1871–1935):
Pioneers of
Organomagnesium Chemistry" (PDF).
Synform. 50: 156–158.[permanent dead link] G. Bram; E. Peralez; J.-C. Negrel; M...
-
Palaeoproterozoic meta-sedimentary and meta-volcanic
rocks that are
preserved in a
synform. The
sequence has been
dated by a
gabbro intrusion,
which gives a date...
- linear,
strata dip away from the
axial center, age unknown, or inverted.
Synform: linear,
strata dip
toward the
axial center, age unknown, or inverted....
- (Lochkovian –
early Emsian)
bioevents and
conodont response in the
Prague Synform (Czech Republic)". Palaeogeography, Palaeoclimatology, Palaeoecology. 549...
-
series of west-plunging
antiforms and
synforms, with
Devonian sediments preserved in four of the
larger synforms as the Solund, Kvamshesten, Håsteinen...
-
Icelandic volcanic rift
zones can be
explained by the rift jump model.
Synform folding is
expected to
occur at the
active rift axis. However, distinctive...
-
whereas a
syncline is its converse; a downfold. Antiforms, anticlinoria,
synforms and
synclinoria are
variations on these. A
monocline (or, rarely, a monoform)...
