-
Flaser beds are a sedimentary, bi-directional,
bedding pattern created when a
sediment is
exposed to
intermittent flows,
leading to
alternating sand and...
- main
types of
heterolithic bedding are
flaser, wavy, and lenticular.
Starved ripples and
cross bedding with
flasers can also be
considered forms of heterolithic...
- crushing. The
granites p**** into
gneiss and granulite; the
gabbros into
flaser gabbro and amphibolite; the
slates often contain andalusite or chiastolite...
- is
classified by its
large quantities of mud
relative to sand,
whereas a
flaser bed
consists mostly of sand. The sand
formations within the
bedding display...
- the
ripple height is
roughly one centimeter. It is lenticular, wavy and
flaser lamination.
Small Small cross-bedding are
ripples set at a
height less than...
- that are
created by
these processes are
herringbone cross-stratification,
flaser bedding, and
interference ripples.
Asymmetrical ripple marks These are created...
-
molar tooth structures, as well as
teepee structures,
desiccation cracks,
flaser bedding, and
other sedimentary structures that
indicate deposition in an...
-
upward in cross-bedded
sandstone and
minor siltstone and
claystone with
flaser or
lenticular bedding that are
interpreted as
tidal flat and
tidal channel...
-
paraconglomerate litharenite layers. In the
lower part of the
formation flaser cross bedding in fine
grained sandstone is
found in abundance,
however a...
- 1038/35086515. PMID 11473309. S2CID 4409161. Pollack, J.; Colburn, D.;
Flaser, F.; Kahn, R.; Carson, C.; Pidek, D. (1979). "Properties and
effects of...
