Academic literature on the topic 'Palaeoshorelines'
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Journal articles on the topic "Palaeoshorelines"
Schuster, Mathieu, Claude Roquin, Philippe Duringer, Michel Brunet, Matthieu Caugy, Michel Fontugne, Hassan Taïsso Mackaye, Patrick Vignaud, and Jean-François Ghienne. "Holocene Lake Mega-Chad palaeoshorelines from space." Quaternary Science Reviews 24, no. 16-17 (September 2005): 1821–27. http://dx.doi.org/10.1016/j.quascirev.2005.02.001.
Full textGulyas, Sandor Jr. "The Palaeogeography of Lake Pannon During Deposition of the Congeria rhomboidea Beds." Geologia Croatica 54, no. 1 (June 30, 2001): 15–26. http://dx.doi.org/10.4154/gc.2001.02.
Full textBernecker, T., and A. D. Partridge. "APPROACHES TO PALAEOGEOGRAPHIC RECONSTRUCTIONS OF THE LATROBE GROUP, GIPPSLAND BASIN, SOUTHEASTERN AUSTRALIA." APPEA Journal 45, no. 1 (2005): 581. http://dx.doi.org/10.1071/aj04044.
Full textMeschis, Marco, Giordano Teza, Enrico Serpelloni, Letizia Elia, Giovanni Lattanzi, Miriana Di Donato, and Silvia Castellaro. "Refining Rates of Active Crustal Deformation in the Upper Plate of Subduction Zones, Implied by Geological and Geodetic Data: The E-Dipping West Crati Fault, Southern Italy." Remote Sensing 14, no. 21 (October 23, 2022): 5303. http://dx.doi.org/10.3390/rs14215303.
Full textEl-Asmar, Hesham M. "Holocene palaeoshorelines along the Manzala lagoon, northeast of the Nile Delta, Egypt." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2002, no. 6 (May 29, 2002): 337–61. http://dx.doi.org/10.1127/njgpm/2002/2002/337.
Full textMargold, Martin, Krister N. Jansson, Arjen P. Stroeven, and John D. Jansen. "Glacial Lake Vitim, a 3000-km3 outburst flood from Siberia to the Arctic Ocean." Quaternary Research 76, no. 3 (November 2011): 393–96. http://dx.doi.org/10.1016/j.yqres.2011.06.009.
Full textCarling, P. A., M. Knaapen, P. Borodavko, J. Herget, I. Koptev, P. Huggenberger, and S. Parnachev. "Palaeoshorelines of glacial Lake Kuray–Chuja, south-central Siberia: form, sediments and process." Geological Society, London, Special Publications 354, no. 1 (2011): 111–28. http://dx.doi.org/10.1144/sp354.7.
Full textCawthra, H., J. Compton, E. Fisher, and C. Marean. "Former land surfaces and palaeoshorelines on the Mossel Bay continental shelf, South Africa." Quaternary International 404 (June 2016): 195. http://dx.doi.org/10.1016/j.quaint.2015.08.161.
Full textLebrec, Ulysse, Rosine Riera, Victorien Paumard, Michael J. O'Leary, and Simon C. Lang. "Morphology and distribution of submerged palaeoshorelines: Insights from the North West Shelf of Australia." Earth-Science Reviews 224 (January 2022): 103864. http://dx.doi.org/10.1016/j.earscirev.2021.103864.
Full textMANVILLE, V., and C. J. N. WILSON. "Interactions between volcanism, rifting and subsidence: implications of intracaldera palaeoshorelines at Taupo volcano, New Zealand." Journal of the Geological Society 160, no. 1 (January 2003): 3–6. http://dx.doi.org/10.1144/0016-764902-103.
Full textDissertations / Theses on the topic "Palaeoshorelines"
Ng, Sin-pan, and 吳善斌. "OSL dating of palaeoshorelines of saline lakes at Inner Mongolia." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B46732883.
Full textBerti, Michael. "The evolution of marginal-marine systems of the Amibberg formation, Karasburg Basin, Southern Namibia: implications for Early-Middle Permian palaeogeography in South Western Gondwana." Thesis, 2015. http://hdl.handle.net/10539/17657.
Full textThe Karasburg Basin is situated in southern Namibia and preserves a heterogeneous succession of Karoo Supergroup strata up to 1000m thick. The uppermost preserved succession in this basin is the Amibberg Formation which is 250m thick and consists of intervals of sandstone, siltstone and mudstone. This study uses facies analysis, sequence stratigraphy and petrography to determine the palaeogeography and provenance for the Amibberg Formation. This is then used to establish environmental variability across the Karasburg – Aranos – Main Karoo basins and to define an equivalent of the Amibberg Formation in the Main Karoo Basin. Detailed stratigraphic logging of five outcrop localities has led to the identification of seven distinct lithofacies and two dominant ichnofacies (Cruziana and Skolithos). These lithofacies include: 1) Massive, laminated and bioturbated mudstones interpreted as offshore deposits (OS); 2) Bioturbated siltstones and sandstones which are representative of offshore-transitional environments (OST); 3) Interbedded sandstones and siltstones also interpreted as offshore-transitional deposits (OST) and generated by river-fed hyperpycnal plumes; 4) Sharp based, massive sandstones interpreted as being deposited on the distal lower shoreface (dLSF); 5) Non-amalgamated hummocky cross-stratified (HCS) and wave rippled sandstones interpreted as distal lower shoreface deposits (dLSF); 6) Amalgamated HCS and wave rippled sandstones interpreted as proximal lower shoreface deposits (pLSF); and 7) Soft-sediment deformed (SSD) sandstones and siltstones occurring in close juxtaposition with dLSF and pLSF deposits. The vertical arrangement of these lithofacies shows a general coarsening and shallowing upward trend. Overall the rocks of the Amibberg Formation consist of wave-dominated shoreface deposits with significant influence by tidal processes. Petrographically, the sandstone samples fall into the class of quartz and feldspathic wackes and are sourced from craton interior provenances. Geochemical analysis of mudstones and nodules indicate high levels of microbial activity under predominantly oxic conditions during the deposition of the Amibberg Formation. Five poorly defined 4th order T-R cycles are observable within the strata of the Amibberg Formation. Large regressive intervals are capped by thin transgressive tracts and these cycles are interpreted to have formed due to eustatic processes. Overall, the Amibberg Formation represents a regressive shoreline. iii Based on the mean palaeocurrent vectors a NNE-SSW palaeoshoreline orientation is deduced and the shoreface must have occupied a palaeohigh on the northern side of the western Cargonian Highlands. This emergent highland acted as an extensive headland and assisted in the connectivity of the Karasburg and Aranos basins, with partial connectivity with the Main Karoo Basin during the Early Permian. Based on this study, the Amibberg Formation is considered an equivalent of the Waterford Formation in the Main Karoo Basin based on similar: stratigraphic position; thickness; sedimentary structures; trace fossil assemblages and stacking patterns.
Book chapters on the topic "Palaeoshorelines"
Feulner, Frederick. "Investigations of Submerged Palaeoshorelines in the Kiel Fjord." In Under the Sea: Archaeology and Palaeolandscapes of the Continental Shelf, 155–63. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53160-1_10.
Full textCastagnino Berlinghieri, Elena Flavia, Fabrizio Antonioli, and Geoff Bailey. "Italy: The Archaeology of Palaeoshorelines, Coastal Caves and Seafaring Connections." In The Archaeology of Europe’s Drowned Landscapes, 321–40. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-37367-2_16.
Full textInglis, Robyn H., William Bosworth, Najeeb M. A. Rasul, Ali O. Al-Saeedi, and Geoff N. Bailey. "Investigating the Palaeoshorelines and Coastal Archaeology of the Southern Red Sea." In Geological Setting, Palaeoenvironment and Archaeology of the Red Sea, 553–81. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99408-6_25.
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