Готові списки джерел за темами / Glacigenes

Добірка наукової літератури з теми "Glacigenes"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 29 січня 2023

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Статті в журналах з теми "Glacigenes"

1

van der Meer, J. J. M. "Glacigenic sediments." Quaternary Science Reviews 11, no. 7-8 (1992): 823–24. http://dx.doi.org/10.1016/0277-3791(92)90088-p.

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2

Hambrey, Michael J. "Glacigenic Sediments." Earth-Science Reviews 33, no. 1 (August 1992): 44–46. http://dx.doi.org/10.1016/0012-8252(92)90072-2.

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3

Santos, Paulo R. "Glacigenic Sediments." Sedimentary Geology 81, no. 1-2 (November 1992): 157–58. http://dx.doi.org/10.1016/0037-0738(92)90063-w.

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4

Menzies, John. "Review of glacigenic sediments." Palaeogeography, Palaeoclimatology, Palaeoecology 102, no. 3-4 (June 1993): 337–39. http://dx.doi.org/10.1016/0031-0182(93)90079-x.

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5

McMillan, A. A. "A provisional Quaternary and Neogene lithostratigraphical framework for Great Britain." Netherlands Journal of Geosciences 84, no. 2 (July 2005): 87–107. http://dx.doi.org/10.1017/s0016774600022988.

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AbstractThis paper presents an overview of a provisional lithostratigraphical framework for the Quaternary and Neogene deposits of Great Britain (England, Scotland and Wales) (onshore). The objective is to provide a workable framework to aid future Quaternary mapping and research, and a stratigraphical scheme capable of use in a wide variety of applications. Using the full hierarchy, a supergroup, group and subgroup lithostratigraphy, based upon the primary mapping unit, the formation, is proposed. It is recommended that some classes of lithogenetically-defined deposits which, at present cannot be accorded formational status, should be assigned informally to one of the proposed groups or subgroups. The framework distinguishes one superficial deposits supergroup within which seven groups are defined: i) Crag Group, marine deposits (Late Pliocene to Early Pleistocene); ii), Dunwich Group, fluvial deposits (pre-Anglian/pre-Elsterian); iii) Residual Deposits Group; iv) British Coastal Deposits Group, coastal and marine deposits (Anglian to Holocene); v) Britannia Catchments Group, fluvial, organic and mass movement deposits (Anglian to Holocene) within broadly defined catchment areas related to Late Devensian to present-day physiography; vi) Albion Glacigenic Group, glacigenic deposits (pre-Devensian/pre-Weichselian), and vii) Caledonia Glacigenic Group, glacigenic deposits (Devensian/Weichselian). North of the Devensian (Weichselian) ice-sheet limit, a series of glacigenic subgroups are defined geographically for the two glacigenic groups on the basis of mappable formations of till. The subgroups include associated formations of glaciofluvial and glaciolacustrine deposits. Consequently some of the glacigenic water-lain units may extend beyond the Devensian limit. Catchment subgroups of the Britannia Catchments Group are proposed for formations and lithogenetic units defined within broad present-day physiographic regions by major river drainage systems that have developed since Middle Pleistocene time. Lithostratigraphical description and correlation of formations will aid the refinement of the proposed framework and enable the development of lithostratigraphical maps and three-dimensional models. As well as offering a unified framework for onshore Quaternary and Neogene deposits the proposed supergroup, group and subgroup structure may prove useful for a wide range of regional applications (e.g. hydrological, hydrogeological, engineering).
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6

Curry, Alastair M., and Colin K. Ballantyne. "Paraglacial Modification of Glacigenic Sediment." Geografiska Annaler, Series A: Physical Geography 81, no. 3 (October 1999): 409–19. http://dx.doi.org/10.1111/j.0435-3676.1999.00070.x.

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7

Park, Adrian F., and Bruce E. Broster. "Influence of glacitectonic fractures on wall failure in open excavations: Heath Steele Mines, New Brunswick, Canada." Canadian Geotechnical Journal 33, no. 5 (November 6, 1996): 720–31. http://dx.doi.org/10.1139/t96-098-319.

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Recognition and detailed mapping of glacigenic fractures and reactivated joints, along with such glacigenic features as striae and till fabrics, prove critical in predicting ground control hazards such as pit wall failure. Following a period of heavy rain in the autumn of 1991, a failure occured on part of the wall of an open-pit mining operation on the Heath Steel Mines property. The failure surfaces bounding the complex landslips of the pit wall were all either original glacigenic fractures or other joints reactivated during Late Wisconsinan glacier overriding. Apart from differential movement, such features include joints filled with coarse sand or clay. Comparaison of the geometry of glacigenic fractures in failed areas with the same features in areas just as densely fractured, but which did not fail, reveal a combination of circumstances where failure was predictable. In this case failure of an unstable rock mass resulted from unfavourable kinematic relationships involving the following: the low strength of clay- and sand-filled joints, the presence of highly permeable and weathered joint conduits, the unfavourable geometry between wall and joint orientation, and an occurrence of increased fluid pressure along the joints from high rainfall that triggered movement. Key words: glacitectonics, geotechnical, wall failure, excavations, rock-quality data, instability.
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8

Pedersen, Schack. "Progressive glaciotectonic deformation in Weichselian and Palaeogene deposits at Feggeklit, northern Denmark." Bulletin of the Geological Society of Denmark 42 (February 1, 1996): 153–74. http://dx.doi.org/10.37570/bgsd-1995-42-13.

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Structural analysis of the glaciotectonic deformations at Feggeklit, Mors, Denmark, provide a unique record of succesive deformation phases in a progressive glaciotectonic deformation. The Feggeklit profile displays glaciotectonically folded, thrust-faulted and sheared Palaeogene diatomite with thin volcanic ash layers, the Fur Formation, overlain by a glacigene succession. The combination of stratigraphical and structural analysis shows that the Feggeklit was affected by three glaciodynamic events. The first event is of Saalian age and is represented by the deposition of a till and the formation of a para-authochthonous glacitectonite in the top of the Fur Formation deposits. The second event is only represented by the deposition of a till, probably of Saalian age. The third event is of Late Weichselian age. It includes: 1) deposition of proglacial glaciolacustrine and -fluvial sediments, 2) the formation of a glaciotectonic unit (the Feggeklit deformation complex) and 3) deposition of a till resting on a tectonic uncon-formity formed subglacially. A detailed structural analysis of the glaciotectonic unit provides a subdivision into five succesive deformation phases. The first four phases are related to the proglacial deformation and comprise 1) anastamosing jointing, 2) conjugate faulting, 3) buckle folding and listric thrust faulting, and 4) large scale ramp thrusting. The final phase (5) is related to subglacial shear deformation and loading which produced an allochthonous diatomiteglacitectonite at the sole of the overlying lodgement till. The formation of the structural complex at Feggeklit was caused by two glaciotectonic mechanisms: 1) a proglacial gravity spreading deformation, and 2) a subglacial cataclastic shearing. The balanced cross-section of the fold structures related to the first deformation mechanism indicates that the detachment of the dislocation is situated below the base of the diatomite formation in the plastic clay at a depth of 80-100 m below the surface. Based on the glaciodynamic analysis and considerations on the dating of regional glacigenic setting the velocity of the advancing ice is estimated at 10 m per year. This advance created the gravity spreading deformation reflected in the glaciotectonic structures preserved in the Feggeklit.
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9

Fitzsimons, Sean, Michael Pollington, and Eric Colhoun. "Palaeomagnetism of New Zealand glacigenic deposits." Exploration Geophysics 24, no. 2 (June 1993): 303–4. http://dx.doi.org/10.1071/eg993303.

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10

Rebesco, M., A. Camerlenghi, and J. Llopart. "Glacigenic debris-flow deposits, Storfjorden Fan." Geological Society, London, Memoirs 46, no. 1 (2016): 373–74. http://dx.doi.org/10.1144/m46.34.

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Дисертації з теми "Glacigenes"

1

Naldrett, Dana L. "Glacigenic clays of the Ottawa Valley." Thesis, University of Ottawa (Canada), 1987. http://hdl.handle.net/10393/5275.

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Nelson, Anna Elizabeth. "A sedimentological investigation of glacigenic deposits in Iceland." Thesis, University of Cambridge, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.613671.

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3

Chaney, Alistair John. "Sedimentology, facies architecture and hydrocarbon potential of the Merrimelia Formation (glacial Permo-Carboniferous), Southern Cooper Basin, South Australia." Thesis, University of Aberdeen, 1990. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU125529.

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Sedimentological analysis of cored sections within the Merrimelia Formation (basal Gidgealpa Group, Cooper Basin, South Australia) reveals a complex glacigenic environment, including glaciolacustrine, deltaic, shorezone, fluvial, aeolian and other associated terrestrial facies (over 20 different facies have been identified). These facies are observed within terminoglacial and proglacial environments and interfinger laterally and vertically constantly throughout the Merrimelia Formation, exhibiting rapid environment change related to the position of ice sheet. Detailed sedimentological and petrographical (Cubitt 1998) analysis suggests that Tirrawarra sandstone-type sandstones facies belong within the Merrimelia depositional realm. Provenance data (Cubitt 1998) indicates that the lithic component of the Tirrawarra Sandstone (sensu stricto), is sourced from reworked Merrimelia coeval depositional facies. It is proposed that the fluvial sandstones of the Merrimelia Formation are part of the same fluvial deposystem as the Tirrawarra Sandstone (sensu stricto) as the two sandstone sequences are the natural progression of coarsening sediment as more detritus was released from melting glaciers during deglaciation. It is suggested that there no longer remain any sedimentological, stratigraphical or petrographical (Cubitt 1998) reasons why the Tirrawarra Sandstone (sensu stricto) and the Merrimelia Formation glaciofluvial sandstones should not be grouped together as Tirrawarra-type facies within the Merrimelia glacigenic domain. Facies architecture across the basin on both field and basin wide scales has identified two regional lacustrine episodes, both of which are followed by a period of lacustrine basin clastic infill. Such cycles represent ice advance and retreat, allowing two deglaciation phases and one ice advance phase to be identified.
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4

Leszczynska, Karolina. "Pleistocene glacigenic deposits in Danbury-Tiptree area, Essex, England." Thesis, University of Cambridge, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.610706.

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5

Edwards, Mark Endaf. "Sedimentology and dating of glacigenic sequences : Eastern Irish Sea Basin." Thesis, Aberystwyth University, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.339787.

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6

Crawford, Kevin Robert. "The late Cenozoic sedimentary record of the Antarctic continental shelf : Prydz Bay, East Antarctica and Weddell Sea, West Antactica." Thesis, Liverpool John Moores University, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.388527.

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7

Grigsby, Nathan. "Evaluating the effect of hyporheic exchange on intake temperatures of open-loop geothermal wells in glacigenic outwash aquifers." Wright State University / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=wright1341855556.

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8

Ferley, Simon Julius John. "An examination of the effects of geological and glacigenic controls on the engineering properties of till using a domain based approach." Thesis, University of Birmingham, 2014. http://etheses.bham.ac.uk//id/eprint/5187/.

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Glacial deposits as a whole are some of the most widespread near surface soils in the northern hemisphere, covering large areas of Canada and the United States, eastern and northern Europe and Asia. In Britain during the final Devensian glaciation, significant accretions of stationary ice developed over most upland areas. The resulting materials derived from the attritional action of the base of the moving ice were deposited as till over approximately 60% of the UK. These soils are generally heterogeneous and unsorted, containing varying proportions of clay to boulder size material. This variation in composition has a commensurate effect on the engineering properties of tills. Commercial investigation data from seven sites in Cumbria overlying different bedrock geology were examined in detail using a variety of statistical and graphical techniques to determine whether differences occurred due to bedrock and glacigenic origin. The results of the data analysis confirm the thesis that the bedrock geology, the history of glacigenic deposition and the post glacial history all affect the geotechnical properties of the resulting till. As a corollary, the commonly used empirical relationship between SPT and shear strength used in deriving undrained shear strength was found not to hold for Cumbrian tills.
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9

Passchier, Sandra. "Sedimentology, mineralogy and geochemistry of the sirius group and other cenozoic glacigenic sediments from Antarctica : implications for climate and ice sheet history /." The Ohio State University, 2000. http://rave.ohiolink.edu/etdc/view?acc_num=osu1488203857248356.

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10

Krbcová, Klára. "Proměnlivost mikromorfologie křemenných zrn glacifluviálních akumulací." Master's thesis, 2013. http://www.nusl.cz/ntk/nusl-330049.

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Micromorphology of glaciofluvial sediments were only partially shown by Mahaney et al. (2001). This paper deals with the main diagnostic textures of glaciofluvial sediments and changes of their micromorphology caused fluvial transport. The samples were collected. All samples were collected by Peter Mida and Martin Hanáček in Svalbard in August 2012. Two glacial samples and six glaciofluvial samples were taken near the glacier Bertilbreen and one glacial sample and seven glaciofluvial samples were taken near the glacier Hørbyebreen. Samples were examined under electron microscope. The correlation analyses was used to set the main glaciofluvial microtextures. Similarity of the samples was tested by one-way ANOVA. Increasing numbers of V-shaped pits, rounded grains, meandering ridges and microblocks are typical for characteristic microtextures of glaciofluvial grains which had greater rate of fluvial transport. But the grains mainly transported by glacier had a greater percentage occurence of subangular grains, straight steps, straight and curved grooves, adhering particles, pitting and V-shaped etch pits. Keywords: exoscopy, quartz grains micromorphology, glaciofluvial sediments
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Книги з теми "Glacigenes"

1

Brodzikowski, Krzysztof. Glacigenic sediments. Amsterdam: Elsevier, 1991.

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2

Brodzikowski, K. Glacigenic sediments. Oxford: Elsevier, 1991.

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3

Brodzikowski, Krzysztof. Glacigenic sediments. Amsterdam: Elsevier, 1991.

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4

Glacigenic Sediments. Elsevier, 1990. http://dx.doi.org/10.1016/s0070-4571(08)x7049-9.

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5

Brodzikowski, K., and A. J. van Loon. Glacigenic Sediments. Elsevier Science & Technology Books, 1990.

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6

Genetic Classification Glacigenic Dep. Taylor & Francis, 1989.

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7

1911-, Goldthwait Richard Parker, Matsch Charles L, and International Union for Quaternary Research. Commission on Genesis and Lithology of Glacial Quaternary Deposits., eds. Genetic classification of glacigenic deposits: Final report of the Commission on Genesis and Lithology of Glacial Quaternary Deposits of the International Union for Quaternary Research (INQUA). Rotterdam: Balkema, 1989.

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Частини книг з теми "Glacigenes"

1

Laberg, Jan Sverre, Runar Johansen, and Stefan Bünz. "A Surging Behaviour of Glacigenic Debris Flows." In Submarine Mass Movements and Their Consequences, 441–50. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-2162-3_39.

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2

Lowrie, Allen, and Karl Hinz. "Glacigenic Sedimentation and Late Neogene Climate Pattern." In Glaciated Continental Margins, 209–12. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_76.

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3

Crane, Kathleen, Peter R. Vogt, and Eirik Sundvor. "Glacigenic Mudflows on the Bear Island Trough Mouth Fan." In Glaciated Continental Margins, 120–21. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_44.

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4

Nygård, A., H. P. Sejrup, and H. Haflidason. "Morphology of Glacigenic Debris Flows on the Upper North Sea Fan." In European Margin Sediment Dynamics, 87–91. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55846-7_13.

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Bacchus, Tania S., and Daniel F. Belknap. "Glacigenic Features and Shelf Basin Stratigraphy of the Eastern Gulf of Maine." In Glaciated Continental Margins, 213–16. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_77.

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6

Vanneste, Kris, Friedrich Theilen, and Heinz Miller. "Large-Scale Stratigraphy of Major Glacigenic Depocenters Along the Polar North Atlantic Margins." In Glaciated Continental Margins, 268–71. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5820-6_91.

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7

Von Brunn, V. "A Facies Analysis of Permo-Carboniferous Glacigenic Deposits Along a Paleoscarp in Northern Natal, South Africa." In Gondwana Six: Stratigraphy, Sedimentology, and Paleontology, 113–22. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm041p0113.

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8

Laberg, J. S., and T. O. Vorren. "Submarine Glacigenic Debris Flows on the Bear Island Trough Mouth Fan, Western Barents Sea: Aspects of Flow Behaviour." In European Margin Sediment Dynamics, 83–85. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55846-7_12.

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9

Nygård, A., H. Haflidason, and H. P. Sejrup. "Morphology of a Non-glacigenic Debris Flow Lobe in the Helland Hansen Area Investigated with 3D Seismic Data." In European Margin Sediment Dynamics, 63–65. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55846-7_8.

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10

Hjelstuen, Berit Oline, and Siv Grinde. "3D Seismic Investigations of Pleistocene Mass Transport Deposits and Glacigenic Debris Flows on the North Sea Fan, NE Atlantic Margin." In Submarine Mass Movements and their Consequences, 265–72. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-20979-1_26.

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Тези доповідей конференцій з теми "Glacigenes"

1

Winsemann, J., L. Pollok, U. Polom, and C. Brandes. "Depositional Architecture of Glacigenic Regressive Deltas." In 74th EAGE Conference and Exhibition incorporating EUROPEC 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20148693.

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2

Wiggins, Tahi, Santiago Munevar Garcia, Allison P. Lepp, and Lauren Simkins. "MORPHOMETRY OF GLACIGENIC LAKES IN NORTH AMERICA." 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-375437.

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Lang, J., and J. Winsemann. "Humpback-dunes and Aggrading Standing Waves - Characteristic Features of Glacigenic Subaqueous Fans." In 74th EAGE Conference and Exhibition incorporating EUROPEC 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20148694.

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Petzold, H., W. Bahrt, M. Bauer, and R. Seitz. "Seismic Investigation of Glacigenous Macro Structures at the Border of a Lignite Deposit." In 60th EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1998. http://dx.doi.org/10.3997/2214-4609.201408404.

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Lang, J., R. J. Dixon, D. P. Le Heron, and J. Winsemann. "Depositional Architecture and Sequence Stratigraphy of Upper Ordovician Glacigenic Deposits, Illizi Basin, Algeria." In 74th EAGE Conference and Exhibition incorporating EUROPEC 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20148830.

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Ives, Libby R. W., and John L. Isbell. "PRELIMINARY SEDIMENTOLOGICAL AND STRATIGRAPHIC ANALYSIS OF THE BASAL GLACIGENIC WYNYARD FORMATION (WYNYARD, TASMANIA, AUSTRALIA)." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-311961.

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Lisin, V. P., B. F. Romanyuk, and R. N. Seredenko. "Glacigenic Factors in the Soil Foundations of Offshore Structures Formation at the South-Eastern Baltic Shelf." In Marine Technologies 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201901828.

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MacLennan, Scott Angus, Michael P. Eddy, Arthur Merschat, Akshay Mehra, Peter W. Crockford, Adam Maloof, C. S. Southworth, and Blair Schoene. "CONSTRAINING LATE TONIAN CLIMATE THROUGH U-PB GEOCHRONOLOGY OF THE GLACIGENIC KONNAROCK FORMATION FROM SOUTHWEST VIRGINIA, USA." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-360006.

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Maher, Anna-Turi, William W. Simpkins, Alyssa Witt, Jared J. Trost, Andrew Berg, and James Stark. "HYDROGEOLOGIC INVESTIGATION OF GROUNDWATER FLOW IN TILL CONFINING BEDS OVERLYING GLACIGENIC AQUIFERS IN SOUTH-CENTRAL AND NORTH-CENTRAL MINNESOTA." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-313001.

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10

Schoenicke, Olaf, Saleh M. Al-Alawi, Ali S. Al-Bemani, Mohammed Z. Kalam, and Xavier Le Varlet. "Preliminary Studies on Using Artificial Neural etworks to Predict Sedimentary Facies of the Permo-Carboniferous Glacigenic Al Khlata Formation, Oman." In Middle East Oil Show and Conference. Society of Petroleum Engineers, 1999. http://dx.doi.org/10.2118/53260-ms.

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Звіти організацій з теми "Glacigenes"

1

Russell, H. A. J., and R. W. C. Arnott. Hydraulic-jump and hyperconcentrated-flow deposits of a glacigenic subaqueous fan: Oak Ridges Moraine, southern Ontario, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/213504.

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2

Stewart, H. A., A. J. Jamieson, C. Ó Cofaigh, and T. Bradwell. Glacigenic debris-flows and down-slope gullies: evidence of a grounded ice margin during past glacials, South Shetland Trench, Antarctica. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/305931.

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3

McMartin, I., J. E. Campbell, P.-M. Godbout, P. Behnia, T. Tremblay, and P. X. Normandeau. High-resolution mapping of glacial landscapes in the north-central portion of the Laurentide Ice Sheet in Nunavut and Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330867.

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Анотація:
A new glacial geomorphology map covers approximately 415,000 km2 in a core region of the Laurentide Ice Sheet in Nunavut. The compilation builds on recent and legacy maps and is supplemented by visual digitization of glacigenic features using high-resolution digital elevation (ArcticDEM) and Landsat 8 images. From this unprecedented, detailed inventory of >156,000 features and >14,000 field observations, we identify various glacial landsystems, many of which are entirely new and others that are significantly modified or updated. These include ice streams, palimpsest ice flows, and areas where basal ice thermal regimes fluctuated between cold-based and warm-based. The GIS data comprise glacial features mapped at original and generalized scales, standardized field datasets and interpreted glacial landsystems. These comprehensive georeferenced datasets can be used to reconstruct the glacial history in the interior portion of the Laurentide Ice Sheet in Nunavut and Northwest Territories and to identify distinct glacial sediment transport paths for applications to mineral exploration.
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