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Hidden Holocene slip along the coastal El Yolki fault in Central Chile and its possible link with megathrust earthquakes

Melnick, Daniel; Hillemann, Christian; Jara-Muñoz, Julius; Garrett, Ed; Cortés-Aranda, Joaquín; Molina, Diego; Tassara, Andrés; Strecker, Manfred R.

Hidden Holocene slip along the coastal El Yolki fault in Central Chile and its possible link with megathrust earthquakes Thumbnail


Authors

Daniel Melnick

Christian Hillemann

Julius Jara-Muñoz

Ed Garrett

Joaquín Cortés-Aranda

Diego Molina

Andrés Tassara

Manfred R. Strecker



Abstract

Megathrust earthquakes are commonly accompanied by increased upper‐plate seismicity and occasionally triggered fault slip. In Chile, crustal faults slipped during and after the 2010 Maule (M8.8) earthquake. We studied the El Yolki fault (EYOF), a transtensional structure midways the Maule rupture not triggered in 2010. We mapped a Holocene coastal plain using LiDAR, which did not reveal surface ruptures. However, the inner‐edge and shoreline angles along the coastal plain as well as 4.3‐4.0 ka intertidal sediments are back‐tilted on the EYOF footwall block, documenting 10 m of vertical displacement. These deformed markers imply ~2 mm/yr throw rate and dislocation models a slip rate of 5.6 mm/yr for the EYOF. In a 5‐m‐deep trench, the Holocene intertidal sediments onlap to five erosive steps, interpreted as staircase wave‐cut landforms formed by discrete events of relative sea‐level drop. We tentatively associated these steps with coseismic uplift during EYOF earthquakes between 4.3 and 4.0 ka. The Maule earthquake rupture may be subdivided into three subsegments based on coseismic slip and gravity anomalies. Coulomb stress transfer models predict neutral stress changes at the EYOF during the Maule earthquake but positive changes for a synthetic slip distribution at the central subsegment. If EYOF earthquakes were triggered by megathrust events, their slip distribution was probably focused in the central subsegment. Our study highlights the millennial variability of crustal faulting and the megathrust earthquake cycle in Chile, with global implications for assessing the hazards posed by hidden but potentially seismogenic coastal faults along subduction zones.

Citation

Melnick, D., Hillemann, C., Jara-Muñoz, J., Garrett, E., Cortés-Aranda, J., Molina, D., …Strecker, M. R. (2019). Hidden Holocene slip along the coastal El Yolki fault in Central Chile and its possible link with megathrust earthquakes. Journal of Geophysical Research. Solid Earth, 124(7), 7280-7302. https://doi.org/10.1029/2018jb017188

Journal Article Type Article
Acceptance Date Jun 13, 2019
Online Publication Date Jul 9, 2019
Publication Date Jul 31, 2019
Deposit Date Jun 25, 2019
Publicly Available Date Jan 9, 2020
Journal Journal of Geophysical Research. Solid Earth
Print ISSN 2169-9313
Publisher American Geophysical Union
Peer Reviewed Peer Reviewed
Volume 124
Issue 7
Pages 7280-7302
DOI https://doi.org/10.1029/2018jb017188

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Copyright Statement
This is the accepted version of the following article: Melnick, Daniel, Hillemann, Christian, Jara-Muñoz, Julius, Garrett, Ed, Cortés-Aranda, Joaquín, Molina, Diego, Tassara, Andrés & Strecker, Manfred R. (2019). Hidden Holocene slip along the coastal El Yolki fault in Central Chile and its possible link with megathrust earthquakes. Journal of Geophysical Research: Solid Earth 124(7): 7280-7302, which has been published in final form at https://doi.org/10.1029/2018JB017188. This article may be used for non-commercial purposes in accordance With Wiley Terms and Conditions for self-archiving.




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