Marine forearc structure of eastern Java and its role in the 1994 Java tsunami earthquake.

Xia, Yueyang, Geersen, Jacob , Klaeschen, Dirk , Ma, Bo , Lange, Dietrich , Riedel, Michael , Schnabel, Michael and Kopp, Heidrun (2021) Marine forearc structure of eastern Java and its role in the 1994 Java tsunami earthquake. Open Access Solid Earth, 12 . pp. 2467-2477. DOI 10.5194/se-12-2467-2021.

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Abstract

We resolve a previously unrecognized shallow subducting seamount from a re-processed multichannel seismic depth image crossing the 1994 M7.8 Java tsunami earthquake slip area. Seamount subduction is related to the uplift of the overriding plate by lateral shortening and vertical thickening, causing pronounced back-thrusting at the landward slope of the forearc high and the formation of splay faults branching off the landward flank of the subducting seamount. The location of the seamount in relation to the 1994 earthquake hypocentre and its co-seismic slip model suggests that the seamount acted as a seismic barrier to the up-dip co-seismic rupture propagation of this moderate size earthquake. The wrapping of the co-seismic slip contours around the seamount indicates that it diverted rupture propagation, documenting the control of forearc structures on seismic rupture.

Document Type: Article
Funder compliance: BMBF:03G0190A ; BMBF:03G0190B
Keywords: Subduction zone, Megathrust earthquake, Seamount subduction, Tsunami earthquake, Multi-channel seismic
Research affiliation: OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Kiel University
Main POF Topic: PT3: Restless Earth
Refereed: Yes
Open Access Journal?: Yes
Publisher: Copernicus Publications (EGU)
Projects: SINDBAD
Expeditions/Models/Experiments:
Date Deposited: 25 May 2021 14:12
Last Modified: 07 Feb 2024 15:27
URI: https://oceanrep.geomar.de/id/eprint/52645

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