Fault Geometry and Slip Distribution at Depth of the 1997 Mw 7.2 Zirkuh Earthquake: Contribution of Near‐Field Displacement Data. Issue 2 (15th February 2018)

• Record Type: Journal Article
• Authors: Marchandon, Mathilde; Vergnolle, Mathilde; Sudhaus, Henriette; Cavalié, Olivier
• Is Part Of: Journal of geophysical research. Volume 123:Issue 2(2018)
• Page Start: 1904
• Page End: 1924
• Publication Date: 2018-02-15
• Subjects: optical correlation data -- Zirkuh strike‐slip earthquake -- shallow slip deficit -- fault slip model -- fault geometry -- Iran; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1002/2017JB014703
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: In this study, we reestimate the source model of the 1997 Mw 7.2 Zirkuh earthquake (northeastern Iran) by jointly optimizing intermediate‐field Interferometry Synthetic Aperture Radar data and near‐field optical correlation data using a two‐step fault modeling procedure. First, we estimate the geometry of the multisegmented Abiz fault using a genetic algorithm. Then, we discretize the fault segments into subfaults and invert the data to image the slip distribution on the fault. Our joint‐data model, although similar to the Interferometry Synthetic Aperture Radar‐based model to the first order, highlights differences in the fault dip and slip distribution. Our preferred model is ∼80° west dipping in the northern part of the fault, ∼75° east dipping in the southern part and shows three disconnected high slip zones separated by low slip zones. The low slip zones are located where the Abiz fault shows geometric complexities and where the aftershocks are located. We interpret this rough slip distribution as three asperities separated by geometrical barriers that impede the rupture propagation. Finally, no shallow slip deficit is found for the overall rupture except on the central segment where it could be due to off‐fault deformation in quaternary deposits. Key Points: Near‐field horizontal surface data contribute assessing complexities in fault geometry and slip distribution Three main segments broke during the earthquake and acted as asperities separated by geometrical barriers where aftershocks are located No shallow slip deficit is found for the overall rupture except on the central segment where it could be due to off‐fault deformation in Quaternary deposits