Academic literature on the topic 'Plio-Pleistocene geomorphology'
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Journal articles on the topic "Plio-Pleistocene geomorphology"
Stuart, Jennifer Y., and Mads Huuse. "3D seismic geomorphology of a large Plio-Pleistocene delta – ‘Bright spots’ and contourites in the Southern North Sea." Marine and Petroleum Geology 38, no. 1 (December 2012): 143–57. http://dx.doi.org/10.1016/j.marpetgeo.2012.06.003.
Full textSmall, David, Michael J. Bentley, David J. A. Evans, Andrew S. Hein, and Stewart P. H. T. Freeman. "Ice-free valleys in the Neptune Range of the Pensacola Mountains, Antarctica: glacial geomorphology, geochronology and potential as palaeoenvironmental archives." Antarctic Science 33, no. 4 (July 5, 2021): 428–55. http://dx.doi.org/10.1017/s0954102021000237.
Full textNiyazi, Yakufu, Mark Warne, and Daniel Ierodiaconou. "Hectometer-scale, shallow buried honeycomb-like structures on the continental shelf of the Otway Basin, southeastern Australia." Interpretation 8, no. 4 (November 1, 2020): SR65—SR81. http://dx.doi.org/10.1190/int-2020-0039.1.
Full textKereszturi, Gábor, Gábor Csillag, Károly Németh, Krisztina Sebe, Kadosa Balogh, and Viktor Jáger. "Volcanic architecture, eruption mechanism and landform evolution of a Plio/Pleistocene intracontinental basaltic polycyclic monogenetic volcano from the Bakony-Balaton Highland Volcanic Field, Hungary." Open Geosciences 2, no. 3 (January 1, 2010). http://dx.doi.org/10.2478/v10085-010-0019-2.
Full textANGULO, Rodolfo José. "MAPA DO CENOZÓICO DO LITORAL DO ESTADO DO PARANÁ." Boletim Paranaense de Geociências 55 (December 31, 2004). http://dx.doi.org/10.5380/geo.v55i0.4281.
Full textDissertations / Theses on the topic "Plio-Pleistocene geomorphology"
Andrews, William M. "Geologic controls on plio-pleistocene draining evolution of the Kentucky river in central Kentucky." Lexington, Ky. : [University of Kentucky Libraries], 2004. http://lib.uky.edu/ETD/ukygeol2004d00169/wmandrews.pdf.
Full textTitle from document title page (October 12, 2004). Document formatted into pages; contains xi, 216 p. : ill., maps. Includes abstract and vita. Includes bibliographical references (p. 202-212).
Pledge, Stephen James. "Tertiary and plio-pleistocene geomorphology and neotectonics of the Nilpena Area, Western Flinders Ranges /." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SB/09sbp7247.pdf.
Full textAndrews, Jr William Morton. "GEOLOGIC CONTROLS ON PLIO-PLEISTOCENE DRAINAGE EVOLUTION OF THE KENTUCKY RIVER IN CENTRAL KENTUCKY." UKnowledge, 2004. http://uknowledge.uky.edu/gradschool_diss/366.
Full textPledge, S. J. "Tertiary and Plio-Pleistocene geomorphology and neotectonics of the Nilpena Area, western Flinders Ranges." Thesis, 2000. http://hdl.handle.net/2440/103500.
Full textThe Nilpena Hills are a small group of low hills extending south from the Ediacara Hills. They are detached from the main Flinders Ranges by an expansive of floodplain about twenty kilometres wide. They consist of uplifted and tilted Precambrian sediments of the Wilpena Group, in particular Pound Subgroup rocks that largely consist of quartzites and sandstones. Surfaces have been interpreted as remnant land surfaces that have been rotated due to the tilting of the Nilpena Hills. These surfaces consist of silcrete skinned cobbles and ironstone stained cobbles, as well as more recent calcrete and gypsum layers. Also in the area are lacustrine sediments. The lacustrine sediments consist of a basal limestone layer, the Nilpena Limestone, and subsequent gypsiferous clays. The age of these lacustrine sediments has been interpreted as Pleistocene and their extents has been mapped. X-ray diffraction analysis was performed on the clays to determine their composition and it was found that some of them contain glauconite. The surfaces also give an important indication of climate in the area and how it has varied from a predominantly warm and wet climate during the formation of the silcretes to a much drier climate during the formation of the ironstone stained cobbled surfaces. Faulting has also played an important part in what is a predominantly extensional area. Reactivation of ancient faults in the late Tertiary or early Quaternary has possibly served as a mechanism for the lake formation. The formation of numerous horsts and grabens in the southern region of the area has also promoted the formation of more armoured surfaces. Faulting in northern area allowed for the generation of a laterite which was subsequently overlain by sand dunes.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2000
"Plio-Pleistocene North-South and East-West Extension at the Southern Margin of the Tibetan Plateau." Doctoral diss., 2012. http://hdl.handle.net/2286/R.I.15099.
Full textDissertation/Thesis
Ph.D. Geological Sciences 2012
Book chapters on the topic "Plio-Pleistocene geomorphology"
"Plio- to Middle Pleistocene Sedimentology, Cave Genesis and Ailsbach Valley Geomorphology." In Famous Planet Earth Caves, edited by Cajus G. Diedrich, 34–53. BENTHAM SCIENCE PUBLISHERS, 2015. http://dx.doi.org/10.2174/9781681080000115010007.
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