A complex earthquake sequence captured by the continuous GPS network in SW Iceland

S. Hreinsdóttir; T. Árnadóttir; J. Decriem; H. Geirsson; A. Tryggvason; R. A. Bennett; P. Lafemina

doi:10.1029/2009GL038391

A complex earthquake sequence captured by the continuous GPS network in SW Iceland

S. Hreinsdóttir
, T. Árnadóttir
, J. Decriem
, H. Geirsson
, A. Tryggvason
, R. A. Bennett
, P. Lafemina

Research output: Contribution to journal › Article › peer-review

39 Scopus citations

Abstract

A complex sequence of earthquakes struck the western part of the South Iceland Scismic Zone (SISZ) on 29 May 2008. The sequence initiated with a M _w6.3 (NEIC) earthquake in the western part of the SISZ. Aftershocks from the earthquake delineate two parallel N-S trending structures 4 km apart, in addition to activity along an E-W zone further westward. Continuous GPS measurements can best be explained by right-lateral strike-slip motion on two parallel N-S trending faults, with little slip occurring on other structures illuminated by earthquake activity. We estimate a total moment release of M _w6.2, with M_w6.1 on the first rupture and M_w6.0 on the second rupture. High rate ( 1 Hz) CGPS data from a near-field station suggest that the main asperity on the Kross fault ruptured within 3 s of the initial mainshock on the Ingólfsfjall fault.

Original language	English (US)
Article number	L12309
Journal	Geophysical Research Letters
Volume	36
Issue number	12
DOIs	https://doi.org/10.1029/2009GL038391
State	Published - Jun 2009

ASJC Scopus subject areas

Geophysics
General Earth and Planetary Sciences

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10.1029/2009GL038391

Cite this

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title = "A complex earthquake sequence captured by the continuous GPS network in SW Iceland",

abstract = "A complex sequence of earthquakes struck the western part of the South Iceland Scismic Zone (SISZ) on 29 May 2008. The sequence initiated with a M w6.3 (NEIC) earthquake in the western part of the SISZ. Aftershocks from the earthquake delineate two parallel N-S trending structures 4 km apart, in addition to activity along an E-W zone further westward. Continuous GPS measurements can best be explained by right-lateral strike-slip motion on two parallel N-S trending faults, with little slip occurring on other structures illuminated by earthquake activity. We estimate a total moment release of M w6.2, with Mw6.1 on the first rupture and Mw6.0 on the second rupture. High rate ( 1 Hz) CGPS data from a near-field station suggest that the main asperity on the Kross fault ruptured within 3 s of the initial mainshock on the Ing{\'o}lfsfjall fault.",

author = "S. Hreinsd{\'o}ttir and T. {\'A}rnad{\'o}ttir and J. Decriem and H. Geirsson and A. Tryggvason and Bennett, \{R. A.\} and P. Lafemina",

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AU - Hreinsdóttir, S.

AU - Árnadóttir, T.

AU - Decriem, J.

AU - Geirsson, H.

AU - Tryggvason, A.

AU - Bennett, R. A.

AU - Lafemina, P.

PY - 2009/6

Y1 - 2009/6

N2 - A complex sequence of earthquakes struck the western part of the South Iceland Scismic Zone (SISZ) on 29 May 2008. The sequence initiated with a M w6.3 (NEIC) earthquake in the western part of the SISZ. Aftershocks from the earthquake delineate two parallel N-S trending structures 4 km apart, in addition to activity along an E-W zone further westward. Continuous GPS measurements can best be explained by right-lateral strike-slip motion on two parallel N-S trending faults, with little slip occurring on other structures illuminated by earthquake activity. We estimate a total moment release of M w6.2, with Mw6.1 on the first rupture and Mw6.0 on the second rupture. High rate ( 1 Hz) CGPS data from a near-field station suggest that the main asperity on the Kross fault ruptured within 3 s of the initial mainshock on the Ingólfsfjall fault.

AB - A complex sequence of earthquakes struck the western part of the South Iceland Scismic Zone (SISZ) on 29 May 2008. The sequence initiated with a M w6.3 (NEIC) earthquake in the western part of the SISZ. Aftershocks from the earthquake delineate two parallel N-S trending structures 4 km apart, in addition to activity along an E-W zone further westward. Continuous GPS measurements can best be explained by right-lateral strike-slip motion on two parallel N-S trending faults, with little slip occurring on other structures illuminated by earthquake activity. We estimate a total moment release of M w6.2, with Mw6.1 on the first rupture and Mw6.0 on the second rupture. High rate ( 1 Hz) CGPS data from a near-field station suggest that the main asperity on the Kross fault ruptured within 3 s of the initial mainshock on the Ingólfsfjall fault.

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JO - Geophysical Research Letters

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A complex earthquake sequence captured by the continuous GPS network in SW Iceland

Abstract

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