Добірка наукової літератури з теми "Antarctica Ross Sea LGM Provenance"
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Статті в журналах з теми "Antarctica Ross Sea LGM Provenance"
Licht, Kathy J., Andrea J. Hennessy, and Bethany M. Welke. "The U-Pb detrital zircon signature of West Antarctic ice stream tills in the Ross embayment, with implications for Last Glacial Maximum ice flow reconstructions." Antarctic Science 26, no. 6 (November 13, 2014): 687–97. http://dx.doi.org/10.1017/s0954102014000315.
Повний текст джерелаPerotti, Matteo, Benedetta Andreucci, Franco Talarico, Massimiliano Zattin, and Antonio Langone. "Multianalytical provenance analysis of Eastern Ross Sea LGM till sediments (Antarctica): Petrography, geochronology, and thermochronology detrital data." Geochemistry, Geophysics, Geosystems 18, no. 6 (June 2017): 2275–304. http://dx.doi.org/10.1002/2016gc006728.
Повний текст джерелаPerotti, Matteo, Luca Zurli, Sonia Sandroni, Gianluca Cornamusini, and Franco Talarico. "Provenance of Ross Sea Drift in McMurdo Sound (Antarctica) and implications for middle-Quaternary to LGM glacial transport: New evidence from petrographic data." Sedimentary Geology 371 (September 2018): 41–54. http://dx.doi.org/10.1016/j.sedgeo.2018.04.009.
Повний текст джерелаLicht, Kathy J., Jason R. Lederer, and R. Jeffrey Swope. "Provenance of LGM glacial till (sand fraction) across the Ross embayment, Antarctica." Quaternary Science Reviews 24, no. 12-13 (July 2005): 1499–520. http://dx.doi.org/10.1016/j.quascirev.2004.10.017.
Повний текст джерелаTolotti, R., C. Salvi, G. Salvi, and M. C. Bonci. "Late Quaternary climate variability as recorded by micropalaeontological diatom data and geochemical data in the western Ross Sea, Antarctica." Antarctic Science 25, no. 6 (March 28, 2013): 804–20. http://dx.doi.org/10.1017/s0954102013000199.
Повний текст джерелаChrist, Andrew J., and Paul R. Bierman. "The local Last Glacial Maximum in McMurdo Sound, Antarctica: Implications for ice-sheet behavior in the Ross Sea Embayment." GSA Bulletin 132, no. 1-2 (May 2, 2019): 31–47. http://dx.doi.org/10.1130/b35139.1.
Повний текст джерелаFinocchiaro, Furio, Carlo Baroni, Ester Colizza, and Roberta Ivaldi. "Pre-LGM open-water conditions south of the Drygalski Ice Tongue, Ross Sea, Antarctica." Antarctic Science 19, no. 3 (July 13, 2007): 373–77. http://dx.doi.org/10.1017/s0954102007000430.
Повний текст джерелаLANGFARMER, G., K. LICHT, R. SWOPE, and J. ANDREWS. "Isotopic constraints on the provenance of fine-grained sediment in LGM tills from the Ross Embayment, Antarctica." Earth and Planetary Science Letters 249, no. 1-2 (September 15, 2006): 90–107. http://dx.doi.org/10.1016/j.epsl.2006.06.044.
Повний текст джерелаBart, Philip J., John B. Anderson, and Frank Nitsche. "Post-LGM Grounding-Line Positions of the Bindschadler Paleo Ice Stream in the Ross Sea Embayment, Antarctica." Journal of Geophysical Research: Earth Surface 122, no. 10 (October 2017): 1827–44. http://dx.doi.org/10.1002/2017jf004259.
Повний текст джерелаAdams, C. J., J. D. Bradshaw, and T. R. Ireland. "Provenance connections between late Neoproterozoic and early Palaeozoic sedimentary basins of the Ross Sea region, Antarctica, south-east Australia and southern Zealandia." Antarctic Science 26, no. 2 (July 18, 2013): 173–82. http://dx.doi.org/10.1017/s0954102013000461.
Повний текст джерелаДисертації з теми "Antarctica Ross Sea LGM Provenance"
Perotti, Matteo. "Provenance of late-Quaternary sediments from Ross Sea region (Antarctica)." Doctoral thesis, Università di Siena, 2018. http://hdl.handle.net/11365/1169858.
Повний текст джерелаTurner, James W. "Dispersal and provenance of fine-grained sediments and the influence of marine transgression on the Ross Sea continental shelf, Antarctica /." The Ohio State University, 1992. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487779439846251.
Повний текст джерелаZurli, Luca. "Provenance analysis of glaciogenic sedimentary formations: cases study from Late Paleozoic Ice Age rocks in Victoria Land (Antarctica) and from Cenozoic DSDP Leg 28 and IODP Expedition 374 cores in the Ross Sea (Antarctica)." Doctoral thesis, Università di Siena, 2022. http://hdl.handle.net/11365/1204543.
Повний текст джерелаThis thesis focus on the provenance study with multidisciplinary approach of sediments and rocks deposited in glacial environments in Antarctica in two distinct temporal contests: the Late Paleozoic Ice Age (LPIA) which involved Gondwana, and the Cenozoic glacial-interglacial cycles. The common point between the two distinct context is the comparison of glacial depositional systems and the provenance study of different temporal, climatic, paleogeographic, and continental settings, whereas both in the Antarctic continent. The comparison could highlight differences between the two studied glacial settings, and it could be useful both for paleo-geographic and paleo-climatic reconstructions and for future previsions. This work is focused on the study of the gravel fraction (clasts larger than 2 mm), constituting glacial sedimentological facies (i.e., diamictite and conglomerate), through petrographic analyses which allow the direct comparison between clasts and outcropping geology of the glacier’s catchments. Other analytical technologies were used to constrain provenance hypothesis based on clast petrography; in particular, chemical analyses on selected mineralogical phases were carried out. These preliminary data seem to show variations in the chemical composition of biotite in intrusive rocks, and it could be used as a marker for the provenance discrimination of intrusive rocks constituting East and West Antarctica. Moreover, geochronological analyses on detrital zircons, from sand size, were carried out; this is an analytical technique largely used for provenance analysis. This technique allows, if applied on fossil systems, the indirect reconstruction of the paleo-tectonic and paleo-morphologic setting of the study region. The methodologies described have been applied in two different cases study extremely different. The first concerns the glacial sediments deposited during the Late Paleozoic Ice Age which currently crop out in Victoria Land (Antarctica); the petrographic and geochronological analyses, coupled with sedimentological and stratigraphic investigations, allow to better define the distribution of the glacial cover across Gondwana in the early Permian, strengthening the hypothesis of multiple and diachronous ice sheets which developed one of the longest glacial phases of the Earth. The second case study is framed inside the IODP Expedition 374, which aims the understanding of the Antarctic Ice sheets dynamics in the Ross Sea (Antarctica) since early Miocene. Gravel sized clasts within sediment cores were identified and described. The clast petrology, compared with ongoing geochronological, geochemical and thermochronological analyses, allows the reconstruction of the paleo-ice flows in the Ross Sea in the early Miocene to Pliocene.
Palmer, Emerson Fowler. "ROCK, TILL, AND ICE: A PROVENANCE STUDY OF THE BYRD GLACIER AND THE CENTRAL AND WESTERN ROSS SEA, ANTARCTICA." Thesis, 2008. http://hdl.handle.net/1805/1631.
Повний текст джерелаDepartment of Earth Sciences, Indiana University-Purdue University Indianapolis (IUPUI). Advisor(s): Kathy J. Licht, Andrew P. Barth, R. Jeffery Swope, Gabriel M. Filippelli. Includes vitae. Includes bibliographical references (leaves 182-191).
Тези доповідей конференцій з теми "Antarctica Ross Sea LGM Provenance"
Christ, Andrew J., and David R. Marchant. "A TERRESTRIAL PERSPECTIVE OF THE LGM IN MCMURDO SOUND, ANTARCTICA: IMPLICATIONS FOR MARINE ICE SHEET DYNAMICS, ICE FLOW, AND DEGLACIATION OF THE ROSS SEA EMBAYMENT." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305311.
Повний текст джерела