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Статті в журналах з теми "Sediments (Geology) Victoria, Southeastern"
Webb, J. A., D. Fabel, B. L. Finlayson, M. Ellaway, Li Shu, and H. P. Spiertz. "Denudation chronology from cave and river terrace levels: the case of the Buchan Karst, southeastern Australia." Geological Magazine 129, no. 3 (May 1992): 307–17. http://dx.doi.org/10.1017/s0016756800019245.
Повний текст джерелаDeev, E. V., I. D. Zolnikov, and S. A. Gus’kov. "Seismites in Quaternary sediments of southeastern Altai." Russian Geology and Geophysics 50, no. 6 (June 2009): 546–61. http://dx.doi.org/10.1016/j.rgg.2008.10.004.
Повний текст джерелаHoldgate, G. R., T. A. G. Smith, S. J. Gallagher, and M. W. Wallace. "Geology of coal-bearing Palaeogene sediments, onshore Torquay Basin, Victoria." Australian Journal of Earth Sciences 48, no. 5 (October 2001): 657. http://dx.doi.org/10.1046/j.1440-0952.2001.00888.x.
Повний текст джерелаHoldgate, G. R., T. A. G. Smith, S. J. Gallagher, and M. W. Wallace. "Geology of coal-bearing Palaeogene sediments, onshore Torquay Basin, Victoria." Australian Journal of Earth Sciences 48, no. 5 (October 2001): 657–79. http://dx.doi.org/10.1046/j.1440-0952.2001.485888.x.
Повний текст джерелаCOLMAN, STEVEN M., ANNE F. CHOQUETTE, JOHN N. ROSHOLT, GIFFORD H. MILLER, and D. J. HUNTLEY. "Dating the upper Cenozoic sediments in Fisher Valley, southeastern Utah." Geological Society of America Bulletin 97, no. 12 (1986): 1422. http://dx.doi.org/10.1130/0016-7606(1986)97<1422:dtucsi>2.0.co;2.
Повний текст джерелаAl-Ankaz, Zinah, Ruaa Muslim, Najah Al-Ghasham, and Hasan Jasim. "Mineral Composition and Provenance of Al-Chabbab Stream Sediments, Wasit, Southeastern Iraq." Iraqi Geological Journal 55, no. 2E (November 30, 2022): 230–42. http://dx.doi.org/10.46717/igj.55.2e.16ms-2022-11-30.
Повний текст джерелаCarranza-Edwards, A., L. Rosales-Hoz, and A. Monreal-Gómez. "Suspended sediments in the southeastern Gulf of Mexico." Marine Geology 112, no. 1-4 (June 1993): 257–69. http://dx.doi.org/10.1016/0025-3227(93)90172-r.
Повний текст джерелаDruzhinina, Olga, Laura Gedminienė, and Kasper van den Berghe. "Metals in Lake Sediments as Indicators of Human Activities in Prehistory: Case Study of the Southeastern Baltic, Kamyshovoe Lake." Minerals 12, no. 10 (September 27, 2022): 1216. http://dx.doi.org/10.3390/min12101216.
Повний текст джерелаEwers Lewis, Carolyn J., Mary A. Young, Daniel Ierodiaconou, Jeffrey A. Baldock, Bruce Hawke, Jonathan Sanderman, Paul E. Carnell, and Peter I. Macreadie. "Drivers and modelling of blue carbon stock variability in sediments of southeastern Australia." Biogeosciences 17, no. 7 (April 16, 2020): 2041–59. http://dx.doi.org/10.5194/bg-17-2041-2020.
Повний текст джерелаFegan, N. E., D. T. Long, W. B. Lyons, M. E. Hines, and P. G. Macumber. "Metal partitioning in acid hypersaline sediments: Lake Tyrrell, Victoria, Australia." Chemical Geology 96, no. 1-2 (March 1992): 167–81. http://dx.doi.org/10.1016/0009-2541(92)90127-q.
Повний текст джерелаДисертації з теми "Sediments (Geology) Victoria, Southeastern"
Sharpe, David Robert. "Glacial sediments and landforms, southern Victoria Island, Northwest Territories, Canada." Thesis, University of Ottawa (Canada), 1992. http://hdl.handle.net/10393/7846.
Повний текст джерелаBasapuram, Laxmi Gayatri Devi. "Lake Victoria - Carbon, Nitrogen, Phosphorus and Stable Isotope (δ13C) comparison between lake and catchment sediments". Thesis, Linköpings universitet, Tema Miljöförändring, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-149283.
Повний текст джерелаLarrahondo-Cruz, Joan Manuel. "Carbonate diagenesis and chemical weathering in the Southeastern United States: some implications on geotechnical behavior." Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/42912.
Повний текст джерелаLe, Roux F. G. "The lithostratigraphy of Cenozoic deposits along the south-east Cape coast as related to sea-level changes." Thesis, Stellenbosch : Stellenbosch University, 1989. http://hdl.handle.net/10019.1/67134.
Повний текст джерелаAFRIKAANSE OPSOMMING: Senosoiese sedimente langs die suidooskus van die Kaapprovinsie is periodiek deur verskeie outeurs vir meer as 'n eeu bestudeer. In hierdie aanbieding word die Iiteratuur saamgevat en vele dubbelsinnige stratigrafiese onderverdelings en definisies opgeklaar. Die Senosoiese afsettings kan volgens oorsprong geklassifiseer word as marien, eolies en fluviaal. Die mariene afsettings, synde strand-, nabystrand-, estuarien of lagunale afsettings geassosieerd met transgressiewe/ regressiewe kusIyne, word nou op grond van kenmerkende litologiese, paleontologiese sowel as ouderdomsverskille onderverdeel in die Paleogeen Bathurst, Neogeen Alexandria en Kwaternere Salnova Foraasies. Die Laat-Plioseen tot Vroeg-Pleistoseen Nanaga Formasie, Middel- tot Laat- Pleistoseen Nahoon Formasie en die Holoseen Schel• Hoek Formasie vorm die kus-eoliese afsettings. AI die mariene en marienverwante (eoliese} formasies, gekenmerk deur kalkige klastiese afsettings, is saamgegroepeer in 'n nuutgedefinieerde Algoa Groep. Fluviale afsettings word onderverdeel in die Martindale, Kinkelbos, Bluewater Bay, Kudus Kloof en Sunland Formasies. Die onderskeie afsettings word gekorreleer met verskillende seevlakstande deur geologiese tye. Die vroegste Senosoiese transgressiewe/regressiewe siklus het in die Vroeg-Paleoseen begin en die hoogste aangetekende elevasie vir die era bereik. Die Bathurst Formasie is waarskynlik gedurende hierdie regressie afgeset. 'n Tweed~ kleiner transgressie/ regressiesiklus het plaasgevind gedurende die Laat-Eoseen tot Vroeg-Oligoseen. Sover tans bekend, kan geen afsetting in die dagsoomgebied van die Algoa Groep definitief met hierdie siklus in verband gebring word nie. Die volgende siklus, wat 'n transgressiewe maksimum van c. 250 m bereik het, het begin in die Middel-Mioseen en verstryk in die Vroee Plioseen. Mariene planasie van die kusplatform het gedurende die transgressie plaasgevind terwyl die Alexandria Formasie wat tans bo 120 m geleë is, gedurende die regressie afgeset is. Die Vroeg-Plioseen transgressie het waarskynlik 'n maksimum huidige hoogte van c. 120 m bereik, waartydens o.a. die 120 m branderstoep en "Humansdorpterras" gekerf is. Die Alexandria Formasie tans geleë tussen 60 en 120 m, is afgeset gedurende die Laat-Plioseen regressie. Hierdie regressie het verskeie relatief lang stilstande, wat waarskynlik die 106-m, 90- tot 100-m en 84-m branderstoepe verklaar, ondervind. Selfs die 60-m en 52-m kuslyne kon tydens hierdie regressie gevorm het. Voorlopige paleontologiese getuienis dui egter daarop dat die 60-m kuslyn 'n transgressiewe maksimum van 'n daaropvolgende siklus verteenwoordig, gevolg deur 'n regressie met minstens een beduidende stilstand by 52 m. Die Alexandria Formasie geleë tussen c. 60 en 30 m, is waarskynlik gedurende hierdie regressie gedeponeer, waartydens ook die Bluewater Bay, Kinkelbos en Kudus Kloof Formasies afgeset is. Gedurende die Kwaternêre transgressie/regressiesiklusse, waarvan minstens vier aangedui word, is die Salnova Formasie (afwesig bo 30 m) afgeset. Die Nahoon Formasie, wat ook op groot skaal op die kontinentale bank ontwikkel is, is gedeponeer gedurende die laaste twee Pleistoseen glasiale toe seevlakke tot benede -100 m gedaal het. Die Schelm Hoek Formasie wat tans nog afgeset word, het ontstaan uit die transgressiewe maksimum van die Flandriese transgressie aan die begin van die Holoseen.
ENGLISH ABSTRACT: Cenozoic sediments along the south-east coast of the Cape Province have been studied intermittently for more than a century by various authors. In this presentation the literature is reviewed and many ambiguous stratigraphic subdivisions and definitions are clarified. The Cenozoic deposits can be classified, according to origin, as marine, aeolian and fluvial. The marine deposits, being lagoonal deposits either beach, nearshore, estuarine or associated with transgressive/regressive shorelines, are now subdivided on the grounds of distinct lithological, palaeontological as well as age differences into the Palaeogene Bathurst, Neogene Alexandria and Quaternary Salnova Formations. The Late Pliocene to Early Pleistocene Nanaga Formation, the Hiddle to Late Pleistocene Nahoon Formation and the Holocene Schelm Hoek Formation constitute the coastal and marine-related aeolian deposits. All the marine (aeolian) formations, which are characterised by calcareous clastics, have been grouped together in a newly defined Algoa Group. Fluvial deposits are subdivided into the Martindale, Kinkelbos, Bluewater Bay, Kudus Kloof and Sunland Formations. The various deposits are correlated with different stands of sea-level through geological time. The earliest Cenozoic transgression/regression cycle started in the Early Palaeocene and reached the highest recorded altitude for the era. The Bathurst Formation was probably deposited during this regression. A second lesser transgression/regression cycle occurred in the Late Eocene to Early Oligocene. As far as is presently known, no deposit in the outcrop area of the Algoa Group can be definitely related to this cycle. The next cycle, which reached a transgressive maximum of c. 250 m, started in the Middle Miocene and terminated in the Early Pliocene. Marine planation of the coastal platform took place during the transgression, whilst the Alexandria Formation presently situated above 120 m, was deposited during the regression. The Early Pliocene transgression is considered to have reached a maximum present-day elevation of c. 120 m, during which the 120 m marine bench and "Humansdorp Terrace", amongst others, were carved. The Alexandria Formation presently situated between 60 and 120 m, was deposited during the Late Pliocene regression, which experienced several relatively long stillstands which probably account for the 106 m, 90 t.o 100 m and 8.4 m benches. Even the 60 m- and 52 m-shorelines could have been formed during this regression. Preliminary palaeontological evidence, however, suggests that the 60 m shoreline represents a transgressive maximum of a subsequent cycle followed by a regression with at least one significant stillstand at 52 m. The Alexandria Formation situated between c. 60 and 30 m, was probably deposited during this regression, which also saw the deposition of the Bluewater Bay, Kinkelbos and Kudus Kloof Formations. During the Quaternary transgression/regression cycles, of which at least four are indicated, the Salnova Formation (absent above 30 m) was deposited. The Nahoon Formation, which is also extensively developed on the continental shelf, was deposited during the last two Pleistocene glacials, when sea-levels receded to less than -100 m. The Schelm Hoek Formation, which is still being deposited, originated from the transgressive maximum of the Flandrian transgression at the start of the Holocene.
Jones, Katie Elizabeth. "Contemporary sediment delivery ratios for small catchments subject to shallow rainfall triggered earthflows in the Waipaoa catchment, North Island, New Zealand : a thesis submitted to the Victoria University of Wellington as partial fulfilment of the requirements for the degree of Master of Science with Honours in Physical Geography /." ResearchArchive@Victoria e-thesis, 2009. http://hdl.handle.net/10063/1197.
Повний текст джерелаGómez-Cabrera, Pedro Tomás. "Stratigraphic and structural analysis of the Neogene sediments of the offshore portion of the Salina del Istmo Basin, southeastern Mexico." Thesis, 2003. http://wwwlib.umi.com/cr/utexas/fullcit?p3119621.
Повний текст джерелаMee, Aija C. "Origin, formation and environmental significance of sapropels in shallow Holocene coastal lakes of Southeastern Australia." 2007. http://hdl.handle.net/2440/57295.
Повний текст джерелаThe aims of this investigation on the Holocene carbonate successions of three shallow, ephemeral lakes from the Cooring coastal plain were: to determine the timing of the sapropel ’events’ in the three lakes; to determine the origin of the sapropelic organic matter and evaluate changes; to establish whether sapropel deposition in these shallow, coastal lakes primarily reflects increased organic matter delivery to the sediments during periods of enhanced terrestrial input and/or aquatic productivity, and; to relate sapropel deposition in these three lakes to both regional and global palaeoenvironment reconstructions. --p. 23-24.
http://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1324064
Thesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2007
Shiga, Yuki. "Dust and terrestrial salt (NaC1) in SE Australia : implications for Aeolian co-transportation and co-deposition." Master's thesis, 2009. http://hdl.handle.net/1885/148226.
Повний текст джерелаDean, C. E. "Lake carbonate geochemistry as a proxy for paleohydrology: a validation-in-time at West Basin Lake, Victoria." Thesis, 2019. https://hdl.handle.net/2440/136950.
Повний текст джерелаThere is a lack of extensive historical climate data in Australia, meaning high-resolution paleoclimate studies are essential for a more comprehensive understanding of natural climate variability. The majority of paleohydrology records in south-eastern Australia region are low resolution, millennial time-scale reconstructions, resulting in a lack of understanding of climate variability at shorter time-scales relevant to human life spans. Here, we attempt to validate the use of geochemical analysis of lake sediments from West Basin, Victoria, as a way to create a high resolution paleohydrology reconstruction. The isotopic composition of the lake water in West Basin is primarily controlled by the precipitation to evaporation ratio (P:E). Ostracod calcite and bulk inorganic carbonates (BIC) that form within the water column reflect these changes and thus are used as proxies of past changes in P:E. This reconstruction is supported by a 210Pb- and 240/230Pu-based chronology which estimates a sediment accumulation rate of 0.3 to 0.4 cm/year and a maximum age at 40 cm of 118 years. This enables the resulting oxygen and carbon profiles to be validated against instrumental records of annual rainfall and temperature. The oxygen profile exhibits good agreement with this climate record, with peaks in δ18O values often coinciding with periods of low annual rainfall. Based on this, the ostracod record was determined to be capable of recording reliable, high resolution changes in P:E. The BIC record, though less consistent, can produce a detailed profile where ostracods are unavailable. Studies of this kind are vital to improving the accuracy of proxy system models which allow for reconstructions to be extended further in the geological record. Such models would allow for contextual understanding of the severity of drought occurrences and the assessment of the possible impacts of human induced climate change.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2019
Книги з теми "Sediments (Geology) Victoria, Southeastern"
Colman, Steven M. Physical, soil, and paleomagnetic stratigraphy of the Upper Cenozoic sediments in Fisher Valley, southeastern Utah. [Washington D.C.]: U.S. G.P.O., 1988.
Знайти повний текст джерелаDyman, T. S. Conglomerate facies and contact relationships of the upper Cretaceous upper part of the Frontier Formation and lower part of the Beaverhead group, Lima Peaks area, southwestern Montana and southeastern Idaho. Washington: U.S. G.P.O., 1995.
Знайти повний текст джерелаKettles, I. M. Composition of glacial sediments in Canadian Shield terrane, southeastern Ontario and southwestern Quebec: Applications to acid rain research and mineral exploration. Ottawa: Geological Survey of Canada, 1994.
Знайти повний текст джерелаClark, David W. Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine Areas, southeastern Montana. Helena, Mont: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.
Знайти повний текст джерелаCanada. Energy, Mines and Resources. Geological Survey ofCanada. Composition of glacial sediments in Canadian Shield terrane, southeastern Ontario and southwestern Quebec: Applications to acid rain research and mineral exploration. Ottawa: Energy, Mines and Resources., 1994.
Знайти повний текст джерелаButler, David L. Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Dolores Project Area, Southwestern Colorado and Southeastern Utah, 1990-91. Denver, Colo: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.
Знайти повний текст джерелаAzza, N. G. T. The Dynamics of Shoreline Wetlands and Sediments of Northern Lake Victoria. Taylor & Francis Ltd, 2006.
Знайти повний текст джерелаSteven, Simpson, Church S. E, and Geological Survey (U.S.), eds. Analytical results and sample locality maps of stream-sediment and rock samples from the Cobblestone Creek area, southeastern Chandler Lake quadrangle, Alaska. [Denver, Colo.]: U.S. Geological Survey, 1989.
Знайти повний текст джерелаSteven, Simpson, Church S. E, and Geological Survey (U.S.), eds. Analytical results and sample locality maps of stream-sediment and rock samples from the Cobblestone Creek area, southeastern Chandler Lake quadrangle, Alaska. [Denver, Colo.]: U.S. Geological Survey, 1989.
Знайти повний текст джерелаN, Haggar Thomas, and University of South Dakota. Science Center., eds. Grain-size analysis of post-cretaceous sand and gravel units in southeastern South Dakota. Vermillion, S.D: Science Center, University of South Dakota, 2002.
Знайти повний текст джерелаТези доповідей конференцій з теми "Sediments (Geology) Victoria, Southeastern"
Self-Trail, Jean, Mercer Parker, David L. Govoni, and Laurel M. Bybell. "RE-EXAMINATION OF UPPER CRETACEOUS AND PALEOGENE FOSSILS AND SEDIMENTS AT THE CABIN BRANCH OUTCROP LOCALITY, MARYLAND: IMPLICATIONS FOR REGIONAL GEOLOGY." In Joint 56th Annual North-Central/ 71st Annual Southeastern Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022nc-373477.
Повний текст джерелаЗвіти організацій з теми "Sediments (Geology) Victoria, Southeastern"
Harrison, J. C., R. L. Christie, R. H. Rainbird, and A. Ford. Geology, tectonic assemblage map of the Cambridge Bay area, southeastern Victoria Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292813.
Повний текст джерелаCaritat, P. de, and U. Troitzsch. Towards a regolith mineralogy map of the Australian continent: a feasibility study in the Darling-Curnamona-Delamerian region. Geoscience Australia, 2021. http://dx.doi.org/10.11636/record.2021.035.
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