The limitations of outcrop must be borne in mind when using these data to interpret paleoslope
, as it is common for ripples in turbidite successions to record directions that differ from the local slope (e.
2009, Permian-Jurassic Mahanadi and Pranhita-Godavari Rifts of Gondwana India: Provenance from regional paleoslope
and U-Pb/Hf analysis of detrital zircons, Gondwana Research, 16, 633-654.
107[degrees]) from a single locality in the Hampton Formation, northeastern Tennessee, and interpreted this to indicate that Chilhowee currents moved primarily down the regional paleoslope
to the southeast.
With this paleoslope
model it was possible to estimate the waterdepth range of many species of benthic foraminifers in the Late Cretaceous Basque-Cantabrian Basin.
Paleoslope is obtained by simplifying the equations governing fluid flow to the case of a steady, horizontally uniform flow in a natural channel, where friction on the walls of the channel is negligible compared to that on the channel bottom.
Reconstructing the flow conditions that resulted in the deposits of the Sharon Formation was accomplished by determining the dimensions of channels, the grain sizes transported by the streams, and the paleoslopes.
Paleoslopes were calculated from solving these equations for slope when the transport stage was set to 1 (initial motion), using paleohydraulic data for bankfull depth, and grain size data (Mohrig 1987; Evans 1991).
Paleoslopes were calculated using the methodology discussed previously.
As this soil gains elevation on the paleoslope
the A horizon disappears and a 3-5 cm thick, dark-red, slightly cemented [B.
The extent of such capping depends not only on the size of the volcano but also on the paleoslope
and duration of the volcanic activity.
1991): A paleoslope
model of late Albian to early Turonian foraminifera of the western Atlantic margin and North Atlantic basin.
Few continuous reflections and variable amplitudes are found on paleoslopes