Under pressure: clastic dykes in glacial settings
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K. Kjær | J. Krüger | J. Meer | J. Rabassa | A. Kilfeather
[1] E. Phillips,et al. Evidence for multiphase water-escape during rafting of shelly marine sediments at Clava, Inverness-shire, NE Scotland , 2008 .
[2] K. Kjær,et al. Instantaneous end moraine and sediment wedge formation during the 1890 glacier surge of Brúarjökull, Iceland , 2008 .
[3] H. French,et al. Water escape fissures resembling ice-wedge casts in Late Quaternay subaquesous outwash near St. Lazare Québec, Canada , 2008 .
[4] B. Broster. Glacitectonic Deformation in Sediment and Bedrock, Hat Creek, British Columbia , 2007 .
[5] N. Eyles,et al. The origin and glaciodynamic significance of sandstone ridge networks from the Hirnantian glaciation of the Djado Basin (Niger) , 2007 .
[6] G. Boulton. Glaciers and their Coupling with Hydraulic and Sedimentary Processes , 2007 .
[7] J. Piotrowski. Groundwater Under Ice Sheets and Glaciers , 2007 .
[8] A. Jain,et al. Liquefaction and fluidization of lacustrine deposits from Lahaul-Spiti and Ladakh Himalaya: Geological evidences of paleoseismicity along active fault zone , 2007 .
[9] K. Kjær,et al. Subglacial decoupling at the sediment/bedrock interface: a new mechanism for rapid flowing ice , 2006 .
[10] P. G. Knight. Glacier science and environmental change , 2006 .
[11] J. Etienne,et al. A complex subglacial clastic dyke swarm, Sólheimajökull, southern Iceland , 2005 .
[12] B. Vliet-Lanoë,et al. Distinguishing between tectonic and periglacial deformations of quaternary continental deposits in Europe , 2004 .
[13] K. Kjær,et al. What causes till thickness to change over distance? Answers from Mýrdalsjökull, Iceland , 2003 .
[14] Ó. Knudsen,et al. Controls on englacial sediment deposition during the November 1996 jökulhlaup, Skeiđarárjökull, Iceland , 2001 .
[15] Ó. Knudsen,et al. Ice fracturing during jökulhlaups: implications for englacial floodwater routing and outlet development , 2000 .
[16] W. Warren,et al. Clastic dykes in over-consolidated tills: evidence for subglacial hydrofracturing at Killiney Bay, eastern Ireland , 1999 .
[17] K. Kjær,et al. Subglacial water escape structures and till structure, Slettjokull, Iceland. , 1999 .
[18] Å. Mattsson. Glacial striae, glacigenous sediments and Weichselian ice movements in southernmost Sweden , 1997 .
[19] W. Warren,et al. The sedimentology of a Late Pleistocene drumlin near Kingscourt, Ireland , 1997 .
[20] A. Dreimanis,et al. Late Wisconsinan sub-glacial clastic intrusive sheets along Lake Erie bluffs, at Bradtville, Ontario, Canada , 1997 .
[21] S. Kluiving. Glaciotectonics of the ltterbeck ‐ Uelsen push moraines, Germany , 1994 .
[22] A. Mccabe,et al. Glaciotectonically induced water-throughflow structures in a Late Pleistocene drumlin, Kanrawer, County Galway, western Ireland , 1994 .
[23] R. Kumpulainen. Fissure-fill and tunnel-fill sediments: expressions of permafrost and increased hydrostatic pressure , 1994 .
[24] J. Mount. Formation of fluidization pipes during liquefaction: examples from the Uratanna Formation (Lower Cambrian), South Australia , 1993 .
[25] A. V. D. Meer,et al. Micromorphological aspects of glaciolacustrine sediments in Northern Patagonia, Argentina , 1992 .
[26] J. Andrews,et al. Tills and Glaciotectonics , 1989 .
[27] S. Y. Johnson. Water-Escape Structures in Coarse-Grained, Volcaniclastic, Fluvial Deposits of the Ellensburg Formation, South-Central Washington , 1986 .
[28] D. Gendzwill,et al. Howe lake: a hydrodynamic blowout structure , 1982 .
[29] J. Meer. The Fribourg area, Switzerland -- a study in Quaternary geology and soil development , 1982 .
[30] H. French. The Periglacial Environment , 1977 .
[31] O. Stephansson,et al. Pre-Holocene joint fillings at Forsmark, Uppland, Sweden , 1975 .
[32] W. Shilts,et al. A Pleistocene Clastic Dike, Upper Chaudière Valley, Québec , 1974 .
[33] J. Goździk,et al. The origin of a giant downward directed clastic dyke in a kame (Bełchatów mine, central Poland) , 2007 .
[34] A. Hałuszczak. Dike-filled extensional structures in Cenozoic deposits of the Kleszczów Graben (Central Poland) , 2007 .
[35] M. Davies,et al. A polar paradise: the glaciation of South Victoria Land, Antarctica , 2004 .
[36] O. Parize,et al. The Vocontian clastic dykes and sills: a geometric model , 2003, Geological Society, London, Special Publications.
[37] J. Menzies. Micromorphological analyses of microfabrics and microstructures indicative of deformation processes in glacial sediments , 2000, Geological Society, London, Special Publications.
[38] Ó. Knudsen,et al. Rapid sediment entrainment and englacial deposition during jökulhlaups , 2000 .
[39] P. M. Maurenbrecher,et al. Liquefaction potential and dewatering injection structures at Herkenbosch: field investigations of the effects of the 1992 Roermond earthquake, the Netherlands , 1996 .
[40] J. Meer. Microscopic evidence of subglacial deformation , 1993 .
[41] J. Mangerud,et al. Subglacially formed clastic dikes , 1992 .
[42] A. Dreimanis. Downward injected till wedges and upward injected till dikes , 1992 .
[43] C. Talbot,et al. Formation and Deformation of Subglacial Intrusive Clastic Sheets in the Dwyka Formation of Northern Natal, South Africa , 1986 .
[44] W. Haeberli,et al. The Uplift of Unteraargletscher at the Beginning of the Melt Season—A Consequence of Water Storage at the Bed? , 1983, Journal of Glaciology.