-
similar to
turbidites.
Turbidites in
sediments can
occur in
carbonate as well as
siliciclastic sequences. classic, low-density
turbidites are characterized...
- replace, the
better known Bouma sequence,
which applies primarily to
turbidites deposited by low-density (i.e., low-sand concentration),
turbidity currents...
- 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...
-
Expedition (NZGSAE) (1964–65). It was
named after sedimentary features,
called turbidites,
which were
reportedly found in
sedimentary rocks of the
Beacon Supergroup...
- and
paleocurrent indicators. Sole
markings are
found most
commonly in
turbidite deposits, but are also
often seen in
modern river beds and
tidal channels...
- such as
Great Bahama Canyon with the
evidence of
turbidity currents and
turbidite deposition.: 33–40, 65, 72–84, 86 The
stratigraphy of the
islands consists...
- convolute-laminated
Bouma C
layers in a
sandy turbidite. Cozy Dell Fm,
Topatopa Mountains, California.
Bouma C-D
layers of
distal turbidites deposited in a
levee crev****e...
-
series of
graded sediments of sand, silt and mud,
which are
known as
turbidites, as
described by the
Bouma sequence. List of
oceanic landforms Gluyas...
- 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...
- (Globigerina ooze) to
silicic mud
lacking carbonates. In rare cases,
turbidites or
other silica-rich
sediments bury and
preserve benthic (deep ocean)...
