Spelling suggestions: "subject:"[een] SEDIMENTATION"" "subject:"[enn] SEDIMENTATION""
1 |
Zur Analyse der Grenzdynamik von stochastischen Vielteilchensystemen am Beispiel des Pickard-Tory-SedimentationsmodellsWittmann, Thorsten. January 2003 (has links) (PDF)
Stuttgart, Universiẗat, Diss., 2003.
|
2 |
Zur Analyse der Grenzdynamik von stochastischen Vielteilchensystemen am Beispiel des Pickard-Tory-Sedimentationsmodells /Wittmann, Thorsten. January 2003 (has links)
Stuttgart, Universiẗat, Diss., 2003.
|
3 |
Land use potimization [sic] and sediment yield model for Siran Watershed (Pakistan)Shah, Bashir Hussain. January 1985 (has links) (PDF)
Thesis (Ph. D. - Renewable Natural Resources)--University of Arizona, 1985. / Includes bibliographical references (leaves 249-252).
|
4 |
A study of sediment deposition in reservoirsMajaj, Nadeem Hana. January 1988 (has links)
Thesis (M.S.)--California State University, Long Beach, 1988. / Photocopy of typescript. Abstract preceding title page. Includes bibliographical references (leaves 99-101).
|
5 |
An improved understanding of shalllow marine depositional systems in extensional basinsCollins, Stephen January 2002 (has links)
No description available.
|
6 |
The sedimentology and uranium mineralization of the Beaufort Group in the Beaufort-West - Fraserburg - Merweville Area, Cape ProvinceKubler, Markus 02 July 2015 (has links)
The sediments of the lower part of the Beaufort Group
(Permian) consist of mudstones, siltstones, fine- to very
Fine-grained sandstones and small amounts of intraformational
conglomerate. The mudstones are generally a
brownish-purple colour, and are massive. The siltstones
are generally greyish-green coloured, and are sometimes
ripple cross-laminated. The sandstones vary in colour
from green to grey. horizontally-bedded, trough cross bedded
and ripple cross-laminated sandstone subfacies
were recognized. All the sandstones found in the area
studied may be described as fine- to very fine-grained,
moderately sorted, arkosic wackes.
The stratigraphic interval studied was found to have a
Thickness of about 850 m. No readily mappable subdivisions
were found. The sandstone to stltstone and mudstone ratio
for the stratigraphic interval is about 1:4.
|
7 |
Sedimentation and accumulation rates of Nazca Plate metalliferous sediments by high resolution Ge(Li) gamma-ray spectrometry of uranium series isotopesMoser, John Christian 21 May 1979 (has links)
Graduation date: 1980
|
8 |
Controls on erodibility in a partially mixed estuary, York River, Virginia /Dickhudt, Patrick J., January 2008 (has links) (PDF)
Thesis (M.Sc.)--College of William and Mary. / Vita. Includes bibliographical references.
|
9 |
A continuation of the study of critical tractive forceConklin, Robert Barron, 1932- January 1964 (has links)
No description available.
|
10 |
Some causes and effects of sedimentation in Clouse Lake /Hahn, Charles Lewis, January 1963 (has links)
Thesis (M.S.)--Ohio State University, 1963. / Includes bibliographical references (leaves 61-63). Available online via OhioLINK's ETD Center
|
Page generated in 0.0414 seconds