%0 Report %1 hjaltadottir_etal:2009 %A Hjaltadóttir, Sigurlaug %A Vogfjörd, Krist'ın S. %A Slunga, Ragnar %C Reykjavik, Iceland %D 2009 %K geophysics seismology %N VI 2009-013 %T Seismic signs of magma pathways through the crust in the Eyjafjallajökull volcano, South Iceland %U http://www.webcitation.org/5p3fKftxd %X Earthquakes recorded in Eyjafjallajökull between 1991 and 2006 by the SIL-network are relocated using a double-difference method and their mechanisms are analysed. Three main swarms occurred during this period, in 1994, 1996, and 1999-2000, two of which were accompanied by surface uplift. The relocated seismic distribution forms an overall pipe-like pattern beneath the northern edge of the ice cap, extends through the crust from the crust-mantle boundary and shows the feeder channel in the volcano. During the latter intrusion swarm (1999-2000) seismicity migrated southwards, towards the centre of uplift. The 1996 swarm occurred at the crust-mantle boundary and indicates a period of magma transport up into the crust from the mantle. The fourth seismic swarm, which occurred in 2009, during preparation of this report, is discussed in Appendix II.

@techreport{hjaltadottir_etal:2009, abstract = {Earthquakes recorded in Eyjafjallaj\"{o}kull between 1991 and 2006 by the SIL-network are relocated using a double-difference method and their mechanisms are analysed. Three main swarms occurred during this period, in 1994, 1996, and 1999-2000, two of which were accompanied by surface uplift. The relocated seismic distribution forms an overall pipe-like pattern beneath the northern edge of the ice cap, extends through the crust from the crust-mantle boundary and shows the feeder channel in the volcano. During the latter intrusion swarm (1999-2000) seismicity migrated southwards, towards the centre of uplift. The 1996 swarm occurred at the crust-mantle boundary and indicates a period of magma transport up into the crust from the mantle. The fourth seismic swarm, which occurred in 2009, during preparation of this report, is discussed in Appendix II.}, added-at = {2012-09-01T13:08:21.000+0200}, address = {Reykjavik, Iceland}, author = {Hjaltad\'{o}ttir, Sigurlaug and Vogfj\"{o}rd, Krist'{\i}n S. and Slunga, Ragnar}, biburl = {https://www.bibsonomy.org/bibtex/2c766e0ce557f828274255fb53d950530/nilsma}, institution = {Vedurstofa Islands / Icelandic Meteorological Office}, interhash = {92cc5ebe5ce2dfe68e96256d3fe69df2}, intrahash = {c766e0ce557f828274255fb53d950530}, issn = {1670-8261}, keywords = {geophysics seismology}, month = dec, number = {VI 2009-013}, timestamp = {2021-02-09T13:26:52.000+0100}, title = {Seismic signs of magma pathways through the crust in the Eyjafjallaj\"{o}kull volcano, South Iceland}, url = {http://www.webcitation.org/5p3fKftxd}, year = 2009 }