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Journal articles on the topic 'Glacimarine'

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Published: 10 December 2022
Last updated: 28 January 2023

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1

Rosa, Kátia Kellem da, Rosemary Vieira, and Jefferson Cardia Simões. "Variabilidade do Processo de Descarga de Água de Degelo Glacial para o Ambiente Glacimarinho da Enseada Martel, ilha Rei George, Antártica (Variability of Water Discharge Process of Melting Ice Environment Glacimarinho of Martel Inlet, Rei George...)." Revista Brasileira de Geografia Física 4, no. 4 (January 22, 2012): 837. http://dx.doi.org/10.26848/rbgf.v4i4.232741.

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A liberação da água estocada no sistema glacial depende da variabilidade da descarga de água de degelo pelas geleiras para o ambiente glacimarinho. Com o processo de retração das geleiras, torna-se importante o monitoramento destes processos. Neste trabalho, a dinâmica hidrológica de geleiras que drenam para a enseada Martel, ilha Rei George, Shetlands do Sul, Antártica, foi investigada através de informações do aporte de água de degelo para o ambiente glacimarinho. Foram realizadas mensurações de vazão no canal proglacial da geleira Wanda e análises da distribuição espacial dos fluxos de água de degelo das geleiras que drenam para a enseada através de técnicas de processamento de imagem ASTER. Resultados demonstram que esses processos liberam um grande fluxo de água de degelo dentro da circulação estuarina, tanto por fluxos em canais proglaciais, provenientes da fusão de geleiras de término terrestre, quanto das geleiras de maré. Esses podem refletir a variabilidade climática evidenciada na área de estudo. Dados demonstraram que há uma correlação direta entre a variabilidade da descarga de água de degelo, a profundidade do perfil do canal proglacial e o aumento da temperatura média do ar local. Assim, o uso desta metodologia possui potencial para o uso no desenvolvimento de modelos de monitoramento da variabilidade dos processos de estocagem de água de degelo. Flutuações nos fluxos de água de degelo podem acarretar mudanças ambientais na dinâmica glacial, na produção de sedimentos glaciais, no nível médio local do mar e nos níveis de salinidade no ambiente glacimarinho.Palavras chaves: estocagem hídrica, mudanças ambientais, descarga de água de degelo, ambiente glacimarinho, canais proglaciais Variability of Water Discharge Process of Melting Ice Environment Glacimarinho of Martel Inlet, Rei George Island, Antarctica ABSTRACTThe release of water storage in glacial system depends on meltwater discharge variability by glacimarine environment. With the glacial retreat, the monitor these processes become relevant for glaciological studies. In this work, the hydrological dynamic of the glaciers with flow for Martel inlet, King George Island, South Shetlands, Antarctica, was investigated through of meltwater contribution date for glacimarine environment. Was performed discharge measurements in proglacial channel at Wanda glacier and analyzed the spatial meltwater contribution of the glaciers in inlet through Aster image processing techniques. Results show that these processes release significantly meltwater flow for Martel inlet by proglacial channels, provided for proglacial terminus glaciers, and tidewater glaciers. These processes can be consequence of climatic variability evidenced in study area. Date show the correlation between the meltwater discharge variability, the proglacial channel profile depth and the air temperate increase. Thus, the application of methodology has potential for variability glacial water storage monitoring studies. Meltwater discharge fluctuations can provide environmental changes in glacial dynamic, glacial sediment yield, level sea and salinity levels in study area.Keywords: water storage, environmental change, melting water discharge, glacimarine environmental, proglacial channel
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2

Powell, Ross D. "Modern Glacimarine Environments." Episodes 10, no. 1 (March 1, 1987): 23–25. http://dx.doi.org/10.18814/epiiugs/1987/v10i1/010.

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3

Gilbert, Robert. "Rafting in glacimarine environments." Geological Society, London, Special Publications 53, no. 1 (1990): 105–20. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.06.

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4

Dowdeswell, Julian A. "Processes of glacimarine sedimentation." Progress in Physical Geography: Earth and Environment 11, no. 1 (March 1987): 52–90. http://dx.doi.org/10.1177/030913338701100103.

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5

Domack, E. W. "Biogenic facies in the Antarctic glacimarine environment: Basis for a polar glacimarine summary." Palaeogeography, Palaeoclimatology, Palaeoecology 63, no. 4 (February 1988): 357–72. http://dx.doi.org/10.1016/0031-0182(88)90105-8.

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6

Andrews, John T., J. A. Dowdeswell, and J. D. Scourse. "Glacimarine Environments: Processes and Sediments." Arctic and Alpine Research 23, no. 4 (November 1991): 456. http://dx.doi.org/10.2307/1551688.

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7

McCarroll, Danny. "Glacimarine Environments: Processes and Sediments." Holocene 2, no. 1 (March 1992): 93. http://dx.doi.org/10.1177/095968369200200117.

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8

PERSSON, KÄRSTIN MALMBERG. "Glacimarine environments: Processes and sediments." Boreas 20, no. 2 (January 16, 2008): 190. http://dx.doi.org/10.1111/j.1502-3885.1991.tb00307.x.

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9

Kehrl, Laura M., Robert L. Hawley, Ross D. Powell, and Julie Brigham-Grette. "Glacimarine sedimentation processes at Kronebreen and Kongsvegen, Svalbard." Journal of Glaciology 57, no. 205 (2011): 841–47. http://dx.doi.org/10.3189/002214311798043708.

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AbstractTidewater glaciers deposit sediment at their terminus, thereby reducing the relative water depth. Reduced water depth can lead to increased glacier stability through decreased rates of iceberg calving, glacier thinning and submarine melting. Here we investigate sedimentation processes at the termini of Kronebreen and Kongsvegen, Svalbard. We mapped the fjord floor bathymetry in August 2009 and calculate sedimentation rates based on our bathymetry and that from a similar study in 2005. A grounding-line fan is developing near the current position of the subglacial stream. An older, abandoned grounding-line fan that likely formed between ∼1987 and 2001 is degrading near the middle of the ice front. Our findings indicate that sediment gravity flows reduce the height of the sediment mound forming at the glacier terminus. The future impact of glacimarine sedimentation processes on glacier stability will depend on the net balance between the observed gravity flows and sediment deposition.
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10

Ó Cofaigh, C., K. A. Hogan, J. A. Dowdeswell, and K. Streuff. "Stratified glacimarine basin-fills in West Greenland fjords." Geological Society, London, Memoirs 46, no. 1 (2016): 99–100. http://dx.doi.org/10.1144/m46.83.

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11

Powell, Ross D., Michael Dawber, James N. McInnes, and Alex R. Pyne. "Observations of the grounding-line area at a floating glacier terminus." Annals of Glaciology 22 (1996): 217–23. http://dx.doi.org/10.3189/1996aog22-1-217-223.

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A robotic submarine was used for the first observations of a grounding-line area of a floating glacier. The site was Mackay Glacier which terminates as a floating glacier tongue in the Ross Sea, at latitude 77°S. Half of the 20 m thick basal debris layers in Mackay Glacier are deposited as subglacial till in the last 1.8 km that the glacier remains grounded. Subglacial till observed at and beyond the grounding line varies rapidly in texture and rheology spatially, occurring as a flat sheet, as flow-parallel flutes, or as bank forms into which it has been pushed at the grounding line. Very little free- flowing subglacial water was present during the observations, and no major subglacial water discharges appear to have occurred in the past. The other half of the basal debris is melted out up to 1.5 km in front of the grounding line, producing a sheet of glacimarine sediment as shelfstone diamicton and mud draped on subglacial till. Both till and glacimarine sediment may be turbated by icebergs. This simple model of till overlain by shelfstone diamicton and mud is a direct contrast to sedimentary depositional systems at tide-water termini of temperate glaciers.
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12

Powell, Ross D., Michael Dawber, James N. McInnes, and Alex R. Pyne. "Observations of the grounding-line area at a floating glacier terminus." Annals of Glaciology 22 (1996): 217–23. http://dx.doi.org/10.1017/s0260305500015457.

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A robotic submarine was used for the first observations of a grounding-line area of a floating glacier. The site was Mackay Glacier which terminates as a floating glacier tongue in the Ross Sea, at latitude 77°S. Half of the 20 m thick basal debris layers in Mackay Glacier are deposited as subglacial till in the last 1.8 km that the glacier remains grounded. Subglacial till observed at and beyond the grounding line varies rapidly in texture and rheology spatially, occurring as a flat sheet, as flow-parallel flutes, or as bank forms into which it has been pushed at the grounding line. Very little free- flowing subglacial water was present during the observations, and no major subglacial water discharges appear to have occurred in the past. The other half of the basal debris is melted out up to 1.5 km in front of the grounding line, producing a sheet of glacimarine sediment as shelfstone diamicton and mud draped on subglacial till. Both till and glacimarine sediment may be turbated by icebergs. This simple model of till overlain by shelfstone diamicton and mud is a direct contrast to sedimentary depositional systems at tide-water termini of temperate glaciers.
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13

Andreassen, Karin, Tore O. Vorren, and Kjell Bugge Johansen. "Pre-Late Weichselian glacimarine sediments at Arnøy, North Norway." Geologiska Föreningen i Stockholm Förhandlingar 107, no. 1 (March 1985): 63–70. http://dx.doi.org/10.1080/11035898509452615.

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14

Rodrigo, Cristian, Andrés Varas-Gómez, Adrián Bustamante-Maino, and Emilio Mena-Hodges. "High-concentration sediment plumes, Horseshoe Island, western Antarctic Peninsula." Antarctic Science 33, no. 2 (March 24, 2021): 213–16. http://dx.doi.org/10.1017/s0954102021000055.

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The variability in sediment concentration and spatial distribution of meltwater discharges from tidewater glaciers can be used to elucidate climatic evolution and glacier behaviour due to the association between sediment yield and glacier retreat (e.g. Domack & McClennen 1996). In an accelerated deglaciation environment, higher sediment concentrations in the water column can change the glacimarine costal dynamics and affect productivity and sea floor ecosystems (e.g. Marín et al. 2013). In the Antarctic Peninsula Region, meltwater or turbid plumes were previously believed to be rare or without an important role in the sedimentary glacimarine environment (e.g. Griffith & Anderson 1989), but recent studies have shown that this is a common phenomenon in subpolar and transition polar climates (Yoo et al. 2015, Rodrigo et al. 2016). In the current climate change scenario, accelerated glacier retreats and mass losses can produce an increasing input of glacial meltwater into the fjord regions, a situation that is not yet well evaluated in the Antarctic Peninsula. In this short note, after in situ observation of an unusual waterfall from the southern side of the main western tidewater glacier (Shoesmith Glacier) of Horseshoe Island (Lystad Bay), Marguerite Bay (Fig. 1), we report high turbidity values associated with plumes from the glacier, whose values were higher than reported data from subpolar/transition polar Antarctic climates.
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15

Dowdeswell, Julian A., and James D. Scourse. "On the description and modelling of glacimarine sediments and sedimentation." Geological Society, London, Special Publications 53, no. 1 (1990): 1–13. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.01.

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16

Berger, G. W., S. Ante, and E. Domack. "Luminescence from glacimarine sediment-trap samples at the Antarctic Peninsula." Quaternary Geochronology 5, no. 2-3 (April 2010): 244–49. http://dx.doi.org/10.1016/j.quageo.2009.01.010.

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17

Ó Cofaigh, C. "Laminated sediments in glacimarine environments: diagnostic criteria for their interpretation." Quaternary Science Reviews 20, no. 13 (July 2001): 1411–36. http://dx.doi.org/10.1016/s0277-3791(00)00177-3.

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18

Streuff, Katharina, Colm Ó Cofaigh, Riko Noormets, and Jeremy M. Lloyd. "Submarine landforms and glacimarine sedimentary processes in Lomfjorden, East Spitsbergen." Marine Geology 390 (August 2017): 51–71. http://dx.doi.org/10.1016/j.margeo.2017.04.014.

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19

Cowan, E. A. "Late Pleistocene glacimarine record in Saanich Inlet, British Columbia, Canada." Marine Geology 174, no. 1-4 (March 2001): 43–57. http://dx.doi.org/10.1016/s0025-3227(00)00141-9.

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20

Gilbert, Robert, Alec E. Aitken, and Donald S. Lemmen. "The glacimarine sedimentary environment of Expedition Fiord, Canadian High Arctic." Marine Geology 110, no. 3-4 (March 1993): 257–73. http://dx.doi.org/10.1016/0025-3227(93)90088-d.

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21

McMillan, A. A., and M. A. E. Browne. "Fold basins in Late–Devensian glacimarine sediments at Shieldhall, Glasgow." Scottish Journal of Geology 25, no. 3 (March 1989): 295–305. http://dx.doi.org/10.1144/sjg25030295.

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22

Stevens, Rodney L. "Proximal and distal glacimarine deposits in southwestern Sweden: contrasts in sedimentation." Geological Society, London, Special Publications 53, no. 1 (1990): 307–16. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.17.

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23

Desloges, Joseph R., Robert Gilbert, Niels Nielsen, Christian Christiansen, Morten Rasch, and Rikke Øhlenschläger. "Holocene glacimarine sedimentary environments in fiords of Disko Bugt, West Greenland." Quaternary Science Reviews 21, no. 8-9 (April 2002): 947–63. http://dx.doi.org/10.1016/s0277-3791(01)00049-x.

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24

DOWDESWELL, J. A., A. ELVERHFI, and R. SPIELHAGEN. "GLACIMARINE SEDIMENTARY PROCESSES AND FACIES ON THE POLAR NORTH ATLANTIC MARGINS." Quaternary Science Reviews 17, no. 1-3 (January 1998): 243–72. http://dx.doi.org/10.1016/s0277-3791(97)00071-1.

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25

Marcos, Paulo, Daniel A. Gregori, Leonardo Benedini, Mercedes Barros, Leonardo Strazzere, and Cecilia Pavón Pivetta. "Pennsylvanian glacimarine sedimentation in the Cushamen Formation, western North Patagonian Massif." Geoscience Frontiers 9, no. 2 (March 2018): 485–504. http://dx.doi.org/10.1016/j.gsf.2017.05.005.

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26

Jaeger, John M. "Developing high-resolution chronologies in glacimarine sediments: examples from southeastern Alaska." Geological Society, London, Special Publications 203, no. 1 (2002): 195–214. http://dx.doi.org/10.1144/gsl.sp.2002.203.01.11.

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27

Rodrigo, Cristian, Andrés Varas, César Grisales, Diana Quintana, and Ricardo Molares. "Glacimarine sediment flows in small bays on the Danco Coast, Antarctic Peninsula." Boletín de Investigaciones Marinas y Costeras 50, SuplEsp (May 26, 2021): 149–68. http://dx.doi.org/10.25268/bimc.invemar.2021.50.suplesp.950.

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Global atmospheric warming and rising ocean temperatures can contribute to the acceleration of glacier melting and influence the generation and physical characteristics of sediment flows in bays and fjords of the Antarctic Peninsula. During the First Scientific Expedition of Colombia to the Antarctic, carried out between January and February 2015, hydrographic variables (temperature, salinity, pressure and turbidity) were measured in the water column, from very close to the main glacier front towards the offshore, on 5 bays of the Danco Coast, Western Antarctic Peninsula. Glacimarine sediment plumes from the tidewater glacier were identified in all bays, however, with varying spatial extensions as well as the concentration of sediments, being those of the central area of the Danco Coast, the most extensive and concentrated. By comparison with previous years, in this work higher average particle concentrations were recorded. The greater flow of glaciomarine sediments could be associated with greater glacial melting, among other possible factors
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28

Cosma, T., and I. L. Hendy. "Pleistocene glacimarine sedimentation on the continental slope off Vancouver Island, British Columbia." Marine Geology 255, no. 1-2 (September 2008): 45–54. http://dx.doi.org/10.1016/j.margeo.2008.07.001.

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29

Gilbert, Robert, Niels Nielsen, Joseph R. Desloges, and Morten Rasch. "Contrasting glacimarine sedimentary environments of two arctic fiords on Disko, West Greenland." Marine Geology 147, no. 1-4 (May 1998): 63–83. http://dx.doi.org/10.1016/s0025-3227(98)00008-5.

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30

Verplanck, Emily P., G. Lang Farmer, John Andrews, Gita Dunhill, and Christian Millo. "Provenance of Quaternary glacial and glacimarine sediments along the southeast Greenland margin." Earth and Planetary Science Letters 286, no. 1-2 (August 2009): 52–62. http://dx.doi.org/10.1016/j.epsl.2009.06.012.

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31

Cowan, Ellen A., Stefanie A. Brachfeld, Ross D. Powell, and Stephanie C. Schoolfield. "Terrane-specific rock magnetic characteristics preserved in glacimarine sediment from southern coastal Alaska." Canadian Journal of Earth Sciences 43, no. 9 (September 1, 2006): 1269–82. http://dx.doi.org/10.1139/e06-042.

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Sediments deposited in three fjord systems latitudinally spanning the northeast Gulf of Alaska coastline have distinctive rock magnetic characteristics that are derived from glacially eroded accreted terranes. Ideal conditions exist in coastal Alaska to preserve primary rock magnetic properties within the sediment record because of the dominance of glacial erosion and rapid sediment transportation and burial. In temperate glacially dominated marine settings, terrigenous sediment is not diluted by biogenic material and diagenetic alteration is minimal. The juxtaposition of temperate glaciers on the northwest-trending accreted terranes of the southern Alaska continental margin provides magnetic provenance tracers of sediment derived from this region that can aid in the interpretation of glacial, paleoclimate, and tectonic proxy records from marine sediment. Holocene sediment deposited in Glacier Bay is eroded from the Craig subterrane of the Alexander terrane; it is characterized by high-volume magnetic susceptibility and coarse-grained, pseudosingle-domain (PSD) and multidomain (MD) magnetite. In Yakutat and Disenchantment bays, farther to the north, glaciers also erode the Yakutat and Chugach terranes. There, sediment contains slightly finer-grained PSD and MD magnetite, which is chemically distinct from that of Glacier Bay. In the northern-most sector, sediment is eroded from the Chugach terrrane in Harriman and College fiords, adjacent to Prince William Sound. These sediments have low magnetic susceptibility and contain micron-size pyrrhotite.
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32

Powell, Ross D. "Glacimarine processes at grounding-line fans and their growth to ice-contact deltas." Geological Society, London, Special Publications 53, no. 1 (1990): 53–73. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.03.

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33

Scourse, J. D., W. E. N. Austin, R. M. Bateman, J. A. Catt, C. D. R. Evans, J. E. Robinson, and J. R. Young. "Sedimentology and micropalaeontology of glacimarine sediments from the Central and Southwestern Celtic Sea." Geological Society, London, Special Publications 53, no. 1 (1990): 329–47. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.19.

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34

Kilfeather, Aoibheann A., Colm Ó Cofaigh, Julian A. Dowdeswell, Jaap J. M. van der Meer, and David J. A. Evans. "Micromorphological characteristics of glacimarine sediments: implications for distinguishing genetic processes of massive diamicts." Geo-Marine Letters 30, no. 2 (September 18, 2009): 77–97. http://dx.doi.org/10.1007/s00367-009-0160-8.

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35

Aitken, Alec E., and Trevor J. Bell. "Holocene glacimarine sedimentation and macrofossil palaeoecology in the Canadian High Arctic: environmental controls." Marine Geology 145, no. 3-4 (March 1998): 151–71. http://dx.doi.org/10.1016/s0025-3227(97)00119-9.

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36

Syvitski, J. P. M., J. T. Andrews, and J. A. Dowdeswell. "Sediment deposition in an iceberg-dominated glacimarine environment, East Greenland: basin fill implications." Global and Planetary Change 12, no. 1-4 (March 1996): 251–70. http://dx.doi.org/10.1016/0921-8181(95)00023-2.

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37

Ó Cofaigh, C., J. T. Andrews, A. E. Jennings, J. A. Dowdeswell, K. A. Hogan, A. A. Kilfeather, and C. Sheldon. "Glacimarine lithofacies, provenance and depositional processes on a West Greenland trough-mouth fan." Journal of Quaternary Science 28, no. 1 (August 24, 2012): 13–26. http://dx.doi.org/10.1002/jqs.2569.

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38

Stewart, F. S. "An evaluation of seismic and borehole data available from onshore and offshore site investigations of relict glaciated areas." Geological Society, London, Engineering Geology Special Publications 7, no. 1 (1991): 573–78. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.56.

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AbstractUsing late Quaternary ice marginal sites from the North Sea and Iceland a comparison of the sedimentary information available from subaerial and submarine site investigations was made. This was with regard to palaeo-environmental reconstructions of ice marginal Sedimentation processes. A detailed high resolution seismic survey in-the North Sea was compared to a similar subaerial site in Iceland. Submarine cores were compared with logged sections available from cliffs. These comparisons highlighted the differences in resolution of the structural information available and also the problems of applying existing modeis of glacimarine Sedimentation to offshore sites. This has raised questions concerning the accuracy of reconstructing palaeo-environments and processes in offshore sites presently under investigation. The implications of this for engineering projects in offshore areas requiring very precise site information about relict glaciated areas are significant.
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39

Ronnert, Lars. "Deposition of fine-grained sediments in a proximal glacimarine environment near Berghem, southwestern Sweden." Geologiska Föreningen i Stockholm Förhandlingar 110, no. 3 (September 1988): 255–62. http://dx.doi.org/10.1080/11035898809455449.

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40

Larsson, Olof, Rodney L. Stevens, and Fredrik Klingberg. "The transition from glacimarine to marine conditions during the last deglaciation in eastern Skagerrak." Marine Geology 241, no. 1-4 (June 2007): 45–61. http://dx.doi.org/10.1016/j.margeo.2007.03.003.

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41

Zecchin, Massimo, and Michele Rebesco. "Glacigenic and glacimarine sedimentation from shelf to trough settings in the NW Barents Sea." Marine Geology 402 (August 2018): 184–93. http://dx.doi.org/10.1016/j.margeo.2018.02.014.

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42

Gilbert, Robert, Niels Nielsen, Henrik Möller, Joseph R. Desloges, and Morten Rasch. "Glacimarine sedimentation in Kangerdluk (Disko Fjord), West Greenland, in response to a surging glacier." Marine Geology 191, no. 1-2 (November 2002): 1–18. http://dx.doi.org/10.1016/s0025-3227(02)00543-1.

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43

Powell, Ross D., and Bruce F. Molnia. "Glacimarine sedimentary processes, facies and morphology of the south-southeast Alaska shelf and fjords." Marine Geology 85, no. 2-4 (January 1989): 359–90. http://dx.doi.org/10.1016/0025-3227(89)90160-6.

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44

Gilbert, Robert, Åsa Chong, Robert B. Dunbar, and Eugene W. Domack. "Sediment Trap Records of Glacimarine Sedimentation at Müller Ice Shelf, Lallemand Fjord, Antarctic Peninsula." Arctic, Antarctic, and Alpine Research 35, no. 1 (February 2003): 24–33. http://dx.doi.org/10.1657/1523-0430(2003)035[0024:strogs]2.0.co;2.

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45

Evans, J., and C. J. Pudsey. "Sedimentation associated with Antarctic Peninsula ice shelves: implications for palaeoenvironmental reconstructions of glacimarine sediments." Journal of the Geological Society 159, no. 3 (May 2002): 233–37. http://dx.doi.org/10.1144/0016-764901-125.

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46

Boulton, G. S. "Sedimentary and sea level changes during glacial cycles and their control on glacimarine facies architecture." Geological Society, London, Special Publications 53, no. 1 (1990): 15–52. http://dx.doi.org/10.1144/gsl.sp.1990.053.01.02.

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47

Milana, Juan Pablo, and Sergio Lopez. "Solar cycles recorded in Carboniferous glacimarine rhythmites (Western Argentina): relationships between climate and sedimentary environment." Palaeogeography, Palaeoclimatology, Palaeoecology 144, no. 1-2 (November 1998): 37–63. http://dx.doi.org/10.1016/s0031-0182(96)00037-5.

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48

Hogan, K. A., J. A. Dowdeswell, and C. Ó Cofaigh. "Glacimarine sedimentary processes and depositional environments in an embayment fed by West Greenland ice streams." Marine Geology 311-314 (May 2012): 1–16. http://dx.doi.org/10.1016/j.margeo.2012.04.006.

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Carr, Simon. "Micromorphological criteria for discriminating subglacial and glacimarine sediments: evidence from a contemporary tidewater glacier, Spitsbergen." Quaternary International 86, no. 1 (December 2001): 71–79. http://dx.doi.org/10.1016/s1040-6182(01)00051-9.

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Cai, Jinkui, Ross D. Powell, Ellen A. Cowan, and Paul R. Carlson. "Lithofacies and seismic-reflection interpretation of temperate glacimarine sedimentation in Tarr Inlet, Glacier Bay, Alaska." Marine Geology 143, no. 1-4 (November 1997): 5–37. http://dx.doi.org/10.1016/s0025-3227(97)00088-1.

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