Crustal deformation at the Sumatran subduction zone revealed by coral rings

Analyses of coral rings grown in the interval 1970–1997 reveal a geographically distinct pattern of interseismic uplift off Sumatra's western coast. At distances less than 110 km from the Sumatran trench, coral reefs are submerging as fast as 5 mm/y. At 130 and 180 km distance from the trench,...

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Main Authors: Ward, Steven N., Natawidjaja, Danny H., Suwargadi, Bambang W., Sieh, Kerry
Format: Article
Language:English
Published: 2012
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Online Access:https://hdl.handle.net/10356/95647
http://hdl.handle.net/10220/8432
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-956472020-09-26T21:38:14Z Crustal deformation at the Sumatran subduction zone revealed by coral rings Ward, Steven N. Natawidjaja, Danny H. Suwargadi, Bambang W. Sieh, Kerry DRNTU::Science::Geology Analyses of coral rings grown in the interval 1970–1997 reveal a geographically distinct pattern of interseismic uplift off Sumatra's western coast. At distances less than 110 km from the Sumatran trench, coral reefs are submerging as fast as 5 mm/y. At 130 and 180 km distance from the trench, they are emerging at similar rates. We suggest that a locked, or partially locked patch, located above 30 km depth on the upper surface of the subducting oceanic plate, generates this pattern. Published version 2012-08-28T06:30:09Z 2019-12-06T19:18:53Z 2012-08-28T06:30:09Z 2019-12-06T19:18:53Z 1999 1999 Journal Article Sieh, K., Ward, S. N., Natawidjaja, D., & Suwargadi, B. W. (1999). Crustal deformation at the Sumatran subduction zone revealed by coral rings. Geophysical Research Letters, 26(20), 3141–3144. https://hdl.handle.net/10356/95647 http://hdl.handle.net/10220/8432 10.1029/1999GL005409 en Geophysical research letters ©1999 American Geophysical Union. This paper was published in Geophysical Research Letters and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The paper can be found at DOI: [http://dx.doi.org/10.1029/1999GL005409]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law. 4 p. application/pdf
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic DRNTU::Science::Geology
spellingShingle DRNTU::Science::Geology
Ward, Steven N.
Natawidjaja, Danny H.
Suwargadi, Bambang W.
Sieh, Kerry
Crustal deformation at the Sumatran subduction zone revealed by coral rings
description Analyses of coral rings grown in the interval 1970–1997 reveal a geographically distinct pattern of interseismic uplift off Sumatra's western coast. At distances less than 110 km from the Sumatran trench, coral reefs are submerging as fast as 5 mm/y. At 130 and 180 km distance from the trench, they are emerging at similar rates. We suggest that a locked, or partially locked patch, located above 30 km depth on the upper surface of the subducting oceanic plate, generates this pattern.
format Article
author Ward, Steven N.
Natawidjaja, Danny H.
Suwargadi, Bambang W.
Sieh, Kerry
author_facet Ward, Steven N.
Natawidjaja, Danny H.
Suwargadi, Bambang W.
Sieh, Kerry
author_sort Ward, Steven N.
title Crustal deformation at the Sumatran subduction zone revealed by coral rings
title_short Crustal deformation at the Sumatran subduction zone revealed by coral rings
title_full Crustal deformation at the Sumatran subduction zone revealed by coral rings
title_fullStr Crustal deformation at the Sumatran subduction zone revealed by coral rings
title_full_unstemmed Crustal deformation at the Sumatran subduction zone revealed by coral rings
title_sort crustal deformation at the sumatran subduction zone revealed by coral rings
publishDate 2012
url https://hdl.handle.net/10356/95647
http://hdl.handle.net/10220/8432
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