Constructing forearc architecture over megathrust seismic cycles: Geological snapshots from the Maule earthquake region, Chile

F Aron, J Cembrano, F Astudillo… - …, 2015 - pubs.geoscienceworld.org
We present new field structural data from the Chilean Coastal Cordillera located above the
northern and central parts of the interplate contact ruptured by the AD 2010 M w 8.8 Maule …

Quantifying offshore fore‐arc deformation and splay‐fault slip using drowned Pleistocene shorelines, Arauco Bay, Chile

J Jara‐Muñoz, D Melnick, P Zambrano… - … research: Solid Earth, 2017 - Wiley Online Library
Most of the deformation associated with the seismic cycle in subduction zones occurs
offshore and has been therefore difficult to quantify with direct observations at millennial …

[PDF][PDF] Splay fault slip during the Mw 8.8 2010 Maule Chile earthquake: REPLY

D Melnick, M Moreno, M Motagh, M Cisternas… - …, 2013 - gfzpublic.gfz-potsdam.de
Originally published as: Melnick, D., Moreno, M., Motagh, M., Cisternas, M., Wesson, RL(2013):
Splay fault sli Page 1 Originally published as: Melnick, D., Moreno, M., Motagh, M., Cisternas …

[HTML][HTML] Crustal Faults Reactivated during 2010 Mw= 8.8 Maule Earthquake in South Chile

J Quezada, A Belmonte - Natural Hazards-New Insights, 2023 - intechopen.com
On February 27th 2010 occurred the Mw= 8.8 Maule subduction earthquake, filling a seismic
gap of south Chile. The uplift trend is mostly typical for subduction earthquakes with …

[HTML][HTML] Quantifying forearc deformation patterns using coastal geomorphic markers: A comprehensive study of marine terraces along the 2010 Maule earthquake (M8 …

J Jara Muñoz - 2016 - publishup.uni-potsdam.de
Rapidly uplifting coastlines are frequently associated with convergent tectonic boundaries,
like subduction zones, which are repeatedly breached by giant megathrust earthquakes …