Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault

Although the 2000‐km‐long Sumatran fault is one of Earth’s longest and historically most active strike‐slip faults, previous large historical ruptures have gone unmapped, although some have been inferred from felt reports or from modeling of sparse geodetic data. Through field observation, we docume...

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Main Authors: Daryono, Mudrik R., Natawidjaja, Danny H., Sieh, Kerry
Format: Journal Article
Language:English
Published: 2013
Online Access:https://hdl.handle.net/10356/101590
http://hdl.handle.net/10220/11153
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author Daryono, Mudrik R.
Natawidjaja, Danny H.
Sieh, Kerry
author_facet Daryono, Mudrik R.
Natawidjaja, Danny H.
Sieh, Kerry
author_sort Daryono, Mudrik R.
collection NTU
description Although the 2000‐km‐long Sumatran fault is one of Earth’s longest and historically most active strike‐slip faults, previous large historical ruptures have gone unmapped, although some have been inferred from felt reports or from modeling of sparse geodetic data. Through field observation, we documented twin‐surface ruptures associated with two M>6 earthquakes in March 2007. The first rupture broke a 22 km part of the 60‐km long Sumani segment southeast from a releasing stepover; the second rupture occurred on a 22.5 km part of the 90‐km‐long Sianok segment northwest from the stepover. Dextral displacements on the two segments averaged 51 and 36 cm. The earlier earthquake doublet in 1926 also straddled this stepover but also did not seem to have ruptured the entire fault segments. Thus, using fault lengths between large stepovers to estimate earthquake magnitude will overestimate what is likely to occur.
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spelling ntu-10356/1015902020-03-07T12:45:26Z Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault Daryono, Mudrik R. Natawidjaja, Danny H. Sieh, Kerry Although the 2000‐km‐long Sumatran fault is one of Earth’s longest and historically most active strike‐slip faults, previous large historical ruptures have gone unmapped, although some have been inferred from felt reports or from modeling of sparse geodetic data. Through field observation, we documented twin‐surface ruptures associated with two M>6 earthquakes in March 2007. The first rupture broke a 22 km part of the 60‐km long Sumani segment southeast from a releasing stepover; the second rupture occurred on a 22.5 km part of the 90‐km‐long Sianok segment northwest from the stepover. Dextral displacements on the two segments averaged 51 and 36 cm. The earlier earthquake doublet in 1926 also straddled this stepover but also did not seem to have ruptured the entire fault segments. Thus, using fault lengths between large stepovers to estimate earthquake magnitude will overestimate what is likely to occur. 2013-07-11T01:52:43Z 2019-12-06T20:40:56Z 2013-07-11T01:52:43Z 2019-12-06T20:40:56Z 2012 2012 Journal Article Daryono, M. R., Natawidjaja, D. H., Sieh, K. (2012). Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault. Bulletin of the Seismological Society of America, 102(6), 2356-2367. https://hdl.handle.net/10356/101590 http://hdl.handle.net/10220/11153 10.1785/0120110220 en Bulletin of the seismological society of America © 2012 Seismological Society of America.
spellingShingle Daryono, Mudrik R.
Natawidjaja, Danny H.
Sieh, Kerry
Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault
title Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault
title_full Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault
title_fullStr Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault
title_full_unstemmed Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault
title_short Twin‐surface ruptures of the March 2007 M>6 earthquake doublet on the Sumatran fault
title_sort twin surface ruptures of the march 2007 m 6 earthquake doublet on the sumatran fault
url https://hdl.handle.net/10356/101590
http://hdl.handle.net/10220/11153
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