Volcano deformation at active plate boundaries

Deep magma accumulation at Hekla volcano and plate boundary deformation in south Iceland

Halldór Geirsson, Peter Lafemina, Thóra Rnadóttir, Erik Sturkell, Freysteinn Sigmundsson, Matthew Travis, Peter Schmidt, Bjorn Lund, Sigrn Hreinsdóttir, Richard A Bennett

Research output: Contribution to journalArticle

26 Citations (Scopus)

Abstract

Most magmatic systems on Earth are located at actively deforming plate boundaries. In these systems, the magmatic and plate boundary deformation signals are intertwined and must be deconvolved to properly estimate magma flux and source characteristics of the magma plumbing system. We investigate the inter-rifting and inter-seismic deformation signals at the Eastern Volcanic Zone (EVZ)-South Iceland Seismic Zone (SISZ) ridge-transform intersection and estimate the location, depth, and volume rate for magmatic sources at Hekla and Torfajkull volcanoes, which are located at the intersection. We solve simultaneously for the source parameters of the tectonic and volcanic deformation signals using a new ten-year velocity field derived from a dense network of episodic and continuous GPS stations in south Iceland. We find the intersection of the axes of the EVZ and the SISZ is located within the Torfajkull caldera, which itself is subsiding. Deformation at Hekla is statistically best described in terms of a horizontal ellipsoidal magma chamber at 24-2+4 km depth aligned with the volcanic system and increasing in volume by 0.017-0.002+0.007 km3 per year. A spherical magma chamber centered at 24-2+5 km depth with a volume rate of 0.019-0.002+0.011 km 3 per year, or a vertical pipe-shaped magma chamber between 10 -1+3 km and 21-4+7 km with a volume rate of 0.008-0.001+0.003 km3 per year are also plausible models explaining the deformation at Hekla. All three models indicate magma accumulation in the lower crust or near the Moho under Hekla.

Original languageEnglish (US)
Article numberB11409
JournalJournal of Geophysical Research: Space Physics
Volume117
Issue number11
DOIs
StatePublished - 2012

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Iceland
Volcanoes
plate boundary
volcanoes
magma
volcano
magma chamber
volcanology
intersections
seismic zone
chambers
Plumbing
source parameters
Tectonics
Moho
caldera
calderas
lower crust
rifting
Global positioning system

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

Volcano deformation at active plate boundaries : Deep magma accumulation at Hekla volcano and plate boundary deformation in south Iceland. / Geirsson, Halldór; Lafemina, Peter; Rnadóttir, Thóra; Sturkell, Erik; Sigmundsson, Freysteinn; Travis, Matthew; Schmidt, Peter; Lund, Bjorn; Hreinsdóttir, Sigrn; Bennett, Richard A.

In: Journal of Geophysical Research: Space Physics, Vol. 117, No. 11, B11409, 2012.

Research output: Contribution to journalArticle

Geirsson, H, Lafemina, P, Rnadóttir, T, Sturkell, E, Sigmundsson, F, Travis, M, Schmidt, P, Lund, B, Hreinsdóttir, S & Bennett, RA 2012, 'Volcano deformation at active plate boundaries: Deep magma accumulation at Hekla volcano and plate boundary deformation in south Iceland', Journal of Geophysical Research: Space Physics, vol. 117, no. 11, B11409. https://doi.org/10.1029/2012JB009400
Geirsson, Halldór ; Lafemina, Peter ; Rnadóttir, Thóra ; Sturkell, Erik ; Sigmundsson, Freysteinn ; Travis, Matthew ; Schmidt, Peter ; Lund, Bjorn ; Hreinsdóttir, Sigrn ; Bennett, Richard A. / Volcano deformation at active plate boundaries : Deep magma accumulation at Hekla volcano and plate boundary deformation in south Iceland. In: Journal of Geophysical Research: Space Physics. 2012 ; Vol. 117, No. 11.
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