-
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...
- 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...
- 677H. doi:10.1038/373677a0. PMID 7854447. Kliore, A. J.; Hinson, D. P.;
Flaser, F. M.; Nagy, A. F.; Cravens, T. E. (18 July 1997). "The
Ionosphere of Europa...
- Hans‐Erich; Wunderlich,
Friedrich (1968). "classification and
Origin of
Flaser and
Lenticular Bedding". Sedimentology. 11 (1–2): 99–104. doi:10.1111/j...
- crushing. The
granites p**** into
gneiss and granulite; the
gabbros into
flaser gabbro and amphibolite; the
slates often contain andalusite or chiastolite...
- that are
created by
these processes are
herringbone cross-stratification,
flaser bedding, and
interference ripples.
Asymmetrical ripple marks These are created...
- near-surface
ground ice.
Nature 412, 411–414 . Pollack, J., D. Colburn, F.
Flaser, R. Kahn, C. Carson, and D. Pidek. 1979.
Properties and
effects of dust...
-
upward in cross-bedded
sandstone and
minor siltstone and
claystone with
flaser or
lenticular bedding that are
interpreted as
tidal flat and
tidal channel...
-
thick clay
dominated heterolites, that
change to more
marine influenced flaser bedded heterolites with some
strongly bioturbated horizons and convolute...
