-
similar to
turbidites.
Turbidites in
sediments can
occur in
carbonate as well as
siliciclastic sequences. classic, low-density
turbidites are characterized...
- submarine-fan
turbidites:
Marine Geology, v. 254, p. 73–90. Huh, C.A., Su, C.C., Liang, W.T., and Ling, C.Y., 2004,
Linkages between turbidites in the southern...
- The
Ozona is
composed of 4 main lithofacies: thick-bedded
turbidites, thin-bedded
turbidites,
mudstone and
conglomeratic mudstone Thick and
thinly bedded...
- replace, the
better known Bouma sequence,
which applies primarily to
turbidites deposited by low-density (i.e., low-sand concentration)
turbidity currents...
-
Expedition (NZGSAE) (1964–65). It was
named after sedimentary features,
called turbidites,
which were
reportedly found in
sedimentary rocks of the
Beacon Supergroup...
- rocks.
Turbidites were
first recognised in the 1950s and the
first facies model was
developed by
Bouma in 1962.
Since that time,
turbidites have been...
- made of
several thin
skinned nappes composed of
Cretaceous to
Paleogene turbidites.
Thrusting of the
Flysch nappes over the
Carpathian foreland caused the...
- composition, the
turbidites have been
divided into
three groups. First,
there are a
group of organic-rich
turbidites.
These turbidites represent organic-rich...
- the
deposition of fine-grained
turbidites and
interseismic sediment deposits through turbidity currents.
These turbidites preserve the
sediment deposits...
- (Globigerina ooze) to
silicic mud
lacking carbonates. In rare cases,
turbidites or
other silica-rich
sediments bury and
preserve benthic (deep ocean)...
