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21 - Indications on Glacially Triggered Faulting in Polar Areas

from Part V - Glacially Triggered Faulting Outside Europe

Published online by Cambridge University Press:  02 December 2021

By
Holger Steffen  and
Rebekka Steffen
Edited by
Holger Steffen ,
Odleiv Olesen  and
Raimo Sutinen
Holger Steffen
Affiliation:
Lantmäteriet, Sweden
Odleiv Olesen
Affiliation:
Geological Survey of Norway
Raimo Sutinen
Affiliation:
Geological Survey of Finland
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Summary

The polar region is the area surrounding the Earth’s geographical poles (Antarctica, Arctic). While glacially induced faults are well known in the formerly glaciated areas of Northern Europe, such faults within the Arctic and Antarctica are unidentified, although the theory of their physical mechanism would allow their presence. Mainly, the fact that most of the polar region is covered either by ocean (Arctic) or ice sheets (Antarctica, Greenland) prevents detailed analysis of those regions with respect to glacially induced faults. However, there are several indications that suggest an existence of glacially induced faults in the polar region. Here, we summarize findings about potential glacially induced faults in Northern Canada, Greenland, Iceland and Svalbard on the northern hemisphere and revisit the seismicity in Antarctica.

Keywords

ArcticAntarcticaCanadaGreenlandIcelandSvalbardBoothia UpliftSeismicityTsunamiRelative Sea Level
Type
Chapter
Information
Glacially-Triggered Faulting , pp. 366 - 380
Publisher: Cambridge University Press
Print publication year: 2021

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References

Adams, R. D., Hughes, A. A. and Zhang, B. M. (1985). A confirmed earthquake in continental Antarctica. Geophysical Journal International, 81(2), 489–492, doi.org/10.1111/j.1365-246X.1985.tb06416.x.CrossRefGoogle Scholar
Arvidsson, R. (1996). Fennoscandian earthquakes: whole crustal rupturing related to postglacial rebound. Science, 274, 744–746, doi.org/10.1126/science.274.5288.744.CrossRefGoogle Scholar
Barletta, V. R., Sørensen, L. S. and Forsberg, R. (2013). Scatter of mass changes estimates at basin scale for Greenland and Antarctica. The Cryosphere, 7, 1411–1432, doi.org/10.5194/tc-7-1411-2013.Google Scholar
Behrendt, J. (1999). Crustal and lithospheric structure of the West Antarctic Rift System from geophysical investigations – a review. Global and Planetary Change, 23, 25–44, doi.org/10.1016/S0921-8181(99)00049-1.CrossRefGoogle Scholar
Brooks, G. R. and Adams, J. (2020). A review of evidence of glacially-induced faulting and seismic shaking in southeastern Canada. Quaternary Science Reviews, 228, 106070, doi.org/10.1016/j.quascirev.2019.106070.Google Scholar
Chung, W.-Y. (2002). Earthquakes along the passive margin of Greenland: evidence for postglacial rebound control. Pure and Applied Geophysics, 159, 2567–2584, doi.org/10.1007/s00024-002-8748-1.Google Scholar
Chung, W.-Y. and Gao, H. (1997). The Greenland earthquake of 11 July 1987 and Postglacial Fault reactivation along a passive margin. Bulletin of the Seismological Society of America, 87(4), 1058–1068.Google Scholar
Clinton, J. F., Nettles, M., Walter, F. et al. (2014). Seismic network in Greenland monitors Earth and ice system. Eos Transactions American Geophysical Union, 95, 13–24, doi.org/10.1002/2014EO020001.Google Scholar
Dörr, N., Clift, P. D., Lisker, F. and Spiegel, C. (2013), Why is Svalbard an island? Evidence for two‐stage uplift, magmatic underplating, and mantle thermal anomalies. Tectonics, 32, 473–486, doi.org/10.1002/tect.20039.Google Scholar
Dyke, A. S. (1998). Holocene delevelling of Devon Island, Arctic Canada: implications for ice sheet geometry and crustal response. Canadian Journal of Earth Sciences, 35, 885–904, doi.org/10.1139/cjes-35-8-885.Google Scholar
Dyke, A. S. (2004). An outline of North American deglaciation with emphasis on central and northern Canada. In Ehlers, J. and Gibbard, P. L., eds., Quaternary Glaciations – Extent and Chronology, Part II. North America., Developments in Quaternary Science 2. Elsevier, New York, pp. 373–424, doi.org/10.1016/S1571-0866(04)80209-4.Google Scholar
Dyke, A. S., Morris, T. F. and Green, D. E. C. (1991). Postglacial Tectonic and Sea Level History of the Central Canadian Arctic. Geological Survey of Canada Bulletin, 397, 56 pp.CrossRefGoogle Scholar
Dyke, A. S., Morris, T. F., Green, D. E. C. and England, J. H. (1992). Quaternary Geology of Prince of Wales Island, Arctic Canada. Geological Survey of Canada Memoir, 433, 142 pp.CrossRefGoogle Scholar
Einarsson, P. (1989). Intraplate earthquakes in Iceland. In Gregersen, S. and Basham, P. W., eds., Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound. Kluwer Academic Press, Dordrecht/Boston/London, pp. 329–344.CrossRefGoogle Scholar
Fenton, C. (1994). Postglacial Faulting in Eastern Canada. Geological Survey of Canada Open File, 2774, 94 pp.Google Scholar
Firth, C. R. and Stewart, I. S. (2000). Postglacial tectonics of the Scottish glacio-isostatic uplift centre. Quaternary Science Reviews, 19, 1469–1493, doi.org/10.1016/S0277-3791(00)00074-3.Google Scholar
Foulger, G. R., Doré, T., Emeleus, C. H. et al. (2020). The Iceland microcontinent and a continental Greenland–Iceland–Faroe Ridge. Earth-Science Reviews, 206, 102926, doi.org/10.1016/j.earscirev.2019.102926.CrossRefGoogle Scholar
Fretwell, P., Pritchard, H. D., Vaughan, D. G. et al. (2013). Bedmap 2: improved ice bed, surface and thickness datasets for Antarctica. The Cryosphere, 7, 375–393, doi.org/10.5194/tc-7-375-2013.Google Scholar
Giardini, D., Grünthal, G., Shedlock, K. M. and Zhang, P. (2003). The GSHAP Global Seismic Hazard Map. In Lee, W., Kanamori, H., Jennings, P. and Kisslinger, C., eds., International Handbook of Earthquake & Engineering Seismology, International Geophysics Series 81B. Academic Press, Amsterdam, pp. 1233–1239.Google Scholar
Goldner, A., Herold, N. and Huber, M. (2014). Antarctic glaciation caused ocean circulation changes at the Eocene–Oligocene transition. Nature, 511(7511), 574–577, doi.org/10.1038/nature13597.Google Scholar
Gregersen, S. (1989). The seismicity of Greenland. In Gregersen, S. and Basham, P.W., eds., Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound. Kluwer Academic Press, Dordrecht/Boston/London, pp. 345–353.CrossRefGoogle Scholar
Gregersen, S. (2006). Intraplate earthquakes in Scandinavia and Greenland. Neotectonics or postglacial uplift. Journal of the Indian Geophysical Union, 10, 25–30.Google Scholar
Henry, C., Das, S. and Woodhouse, J. H. (2000). The March 25, 1998 Mw = 8.1 Antarctic Plate earthquake: moment tensor and rupture history. Journal of Geophysical Research Solid Earth, 105, 16097–16119, doi.org/10.1029/2000JB900077.Google Scholar
Hjartardóttir, Á. R., Einarsson, P. and Brandsdóttir, B. (2011). The Kerlingar fault, Northeast Iceland: a Holocene normal fault east of the divergent plate boundary. Jökull, 60, 103–116.Google Scholar
Hughes, A. L. C., Gyllencreutz, R., Lohne, Ø. S., Mangerud, J. and Svendsen, J. I. (2016). The last Eurasian ice sheets – a chronological database and time-slice reconstruction, DATED-1. Boreas, 45(1), 1–45, doi.org/10.1111/bor.12142.Google Scholar
Ivins, E. R., James, T. S. and Klemann, V. (2003). Glacial isostatic stress shadowing by the Antarctic Ice Sheet. Journal of Geophysical Research Solid Earth, 108(B12), doi.org/10.1029/2002LB002182.Google Scholar
Jacob, T., Wahr, J., Pfeffer, W. T. and Swenson, S. (2012). Recent contributions of glaciers and ice caps to sea level rise. Nature, 482, 514–518, doi.org/10.1038/nature10847.Google Scholar
Johnston, A. C. (1987). Suppression of earthquakes by large continental ice sheets. Nature, 330, 467–469, doi.org/10.1038/330467a0.CrossRefGoogle Scholar
Johnston, A. C. (1996). A wave in the Earth. Science, 274, p. 735, 10.1126/science.274.5288.735.Google Scholar
Jones, S. (1997). Late Quaternary faulting and neotectonics. South Victoria Land, Antarctica. Journal of the Geological Society of London, 153, 645–653, doi.org/10.1144/gsjgs.154.4.0645.Google Scholar
Kaufmann, G., Wu, P. and Ivins, E. R. (2005). Lateral viscosity variations beneath Antarctica and their implications on regional rebound motions and seismotectonics. Journal of Geodynamics, 39, 165–181, doi.org/10.1016/j.jog.2004.08.009.Google Scholar
King, M. A. and Santamaría-Gómez, A. (2016). Ongoing deformation of Antarctica following recent Great Earthquakes. Geophysical Research Letters, 43, 1918–1927, doi.org/10.1002/2016GL067773.CrossRefGoogle Scholar
Kreemer, C. and Holt, W. E. (2000). What caused the March 25, 1998 Antarctic plate earthquake?: inferences from regional stress and strain rate fields. Geophysical Research Letters, 27, 2297–2300, doi.org/10.1029/1999GL011188.CrossRefGoogle Scholar
Kujansuu, R. (1964). Nuorista siirroksista Lapissa [English summary: Recent faults in Lapland]. Geologi, 16, 30–36 (in Finnish).Google Scholar
Lagerbäck, R. and Sundh, M. (2008). Early Holocene Faulting and Paleoseismicity in Northern Sweden. Geological Survey of Sweden Research Paper, Series C, Vol. 836, 80 pp.Google Scholar
Lecavalier, B. S., Milne, G. A., Simpson, M. J. R. et al. (2014). A model of Greenland ice sheet deglaciation constrained by observations of relative sea level and ice extent. Quaternary Science Reviews, 102, 54–84, doi.org/10.1016/j.quascirev.2014.07.018.Google Scholar
Lough, A. C., Wiens, D. A. and Nyblade, A. (2018). Reactivation of ancient Antarctic rift zones by intraplate seismicity. Nature Geoscience, 11(7), 515–519, doi.org/10.1038/s41561-018-0140-6.Google Scholar
Motazedian, D. and Ma, S. (2018). Source parameter studies on the 8 January 2017 Mw 6.1 Resolute, Nunavut, Canada, Earthquake. Seismological Research Letters, 89, 1030–1039, doi.org/10.1785/0220170260.Google Scholar
Munier, R. and Fenton, C. (2004). Review of postglacial faulting. In R. Munier and H. Hökmark, eds., Respect Distances. SKB Technical Report TR-04-17, Swedish Nuclear Fuel and Waste Management Co., Stockholm, pp 157–218.Google Scholar
Olesen, O., Blikra, L. H., Braathen, A. et al.(2004). Neotectonic deformation in Norway and its implications: a review. Norwegian Journal of Geology, 84, 3–34.Google Scholar
Olesen, O., Bungum, H., Dehls, J. et al. (2013). Neotectonics, seismicity and contemporary stress field in Norway – mechanisms and implications. In Olsen, L., Fredin, O. and Olesen, O., eds., Quaternary Geology of Norway, Geological Survey of Norway Special Publication, Vol. 13. pp. 145–174.Google Scholar
Olivieri, M. and Spada, G. (2015). Ice melting and earthquake suppression in Greenland. Polar Science, 9, 94–106, doi.org/10.1016/j.polar.2014.09.004.CrossRefGoogle Scholar
Peulvast, J.-P., Bonow, J. M., Japsen, P., Wilson, R. W. and McCaffrey, K. J. W. (2011). Morphostructural patterns and landform generations in a glaciated passive margin: the Kobberminebugt-Qaqortoq region of South Greenland. Geodinamica Acta, 24(1), 1–19, doi.org/10.3166/ga.24.1-19.CrossRefGoogle Scholar
Piepjohn, K. (1994). Tektonische Evolution der Devongräben (Old Red) in NW-Svalbard [Tectonic evolution of Devonian graben (Old Red) in NW Svalbard]. Unpublished PhD thesis, Westfälische Wilhelms-Universität, Münster, 170 pp.Google Scholar
Roy, K. and Peltier, W. R. (2018). Relative sea level in the Western Mediterranean basin: a regional test of the ICE-7G_NA (VM7) model and a constraint on Late Holocene Antarctic deglaciation. Quaternary Science Reviews, 183, 76–87, doi.org/10.1016/j.quascirev.2017.12.021.Google Scholar
Seierstadt, I., Abbott, P. M., Bigler, M. et al. (2014). Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint. Quaternary Science Reviews, 106, 29–46, doi.org/10.1016/j.quascirev.2014.10.032.Google Scholar
Shepherd, A., Ivins, E., Rignot, E. et al. (2020). Mass balance of the Greenland Ice Sheet from 1992 to 2018. Nature, 579, 233–239 doi.org/10.1038/s41586-019-1855-2.Google Scholar
Simon, K. M., James, T. S., Henton, J. A. and Dyke, A. S. (2016). A glacial isostatic adjustment model for the central and northern Laurentide Ice Sheet based on relative sea-level and GPS measurements. Geophysical Journal International, 205, 1618–1636, doi.org/10.1093/gji/ggw103.Google Scholar
Steffen, H. and Wu, P. (2011). Glacial isostatic adjustment in Fennoscandia – a review of data and modeling. Journal of Geodynamics, 52, 169–204, doi.org/10.1016/j.jog.2011.03.002.Google Scholar
Steffen, R., Steffen, H., Weiss, R. et al. (2020). Early Holocene Greenland-ice mass loss likely triggered earthquakes and tsunami. Earth and Planetary Science Letters, 546, 116443, doi.org/10.1016/j.epsl.2020.116443.Google Scholar
Svendsen, J. I. and Mangerud, J. (1997). Holocene glacial and climatic variations on Spitsbergen, Svalbard. Holocene, 7, 45–57, doi.org/10.1177%2F095968369700700105.Google Scholar
Thiede, J., Jessen, C., Knutz, P. et al. (2011). Millions of years of Greenland Ice Sheet history recorded in ocean sediments. Polarforschung, 80(3), 141–159, doi.org/10.2312/polarforschung.80.3.141.Google Scholar
Tsuboi, S., Kikuchi, M., Yamanaka, Y. and Kanao, M. (2000). The March 25, 1998 Antarctic earthquake: great earthquake caused by postglacial rebound. Earth Planets Space, 52, 133–136, doi.org/10.1186/BF03351621.Google Scholar
van den Heuvel, F., Hübner, C., Błaszczyk, M., Heimann, M. and Lihavainen, H. (2020). SESS Report 2019 – The State of Environmental Science in Svalbard – An Annual Report. Svalbard Integrated Arctic Earth Observing System, Longyearbyen.Google Scholar
Voss, P., Kildegaard Poulsen, S., Simonsen, S. and Gregersen, S. (2007). Seismic hazard assessment of Greenland. GEUS Bulletin, 13, 57–60.CrossRefGoogle Scholar
Wessel, P., Smith, W. H. F., Scharroo, R., Luis, J. F. and Wobbe, F. (2013). Generic Mapping Tools: improved version released. Eos Transactions American Geophysical Union, 94, 409–410, doi.org/10.1002/2013EO450001.CrossRefGoogle Scholar
Wu, P. and Hasegawa, H. S. (1996a). Induced stresses and fault potential in eastern Canada due to a disc load: a preliminary analysis. Geophysical Journal International, 125, 415–430, doi.org/10.1111/j.1365-246X.1996.tb00008.x.Google Scholar
Wu, P. and Hasegawa, H. S. (1996b). Induced stresses and fault potential in Eastern Canada due to a realistic load: a preliminary analysis. Geophysical Journal International, 127, 215–229, doi.org/10.1111/j.1365-246X.1996.tb01546.x.Google Scholar
Yau, A. M., Bender, M. L., Blunier, T. and Jouzel, J. (2016). Setting a chronology for the basal ice at Dye-3 and GRIP: implications for the long-term stability of the Greenland Ice Sheet. Earth and Planetary Science Letters, 451, 1–9, doi.org/10.1016/j.epsl.2016.06.053.Google Scholar

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