Control of décollement strength and dip on fault vergence in fold-thrust belts and accretionary prisms
Author:
Funder
Japan Society for the Promotion of Science
Japan Agency for Marine-Earth Science and Technology
RWTH Aachen University
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference72 articles.
1. Upward delamination of Cascadia Basin sediment infill with landward frontal accretion thrusting caused by rapid glacial age material flux;Adam;Tectonics,2004
2. Control of fault weakening on the structural styles of underthrusting-dominated non-cohesive accretionary wedges;Bauville;J. Geophys. Res. Solid Earth,2020
3. Slip-partitioning above a shallow, weak décollement beneath the Indo-Burman accretionary prism;Betka;Earth Planet. Sci. Lett.,2018
4. Deformation patterns and structural vergence in brittle–ductile thrust wedges: an additional analogue modelling perspective;Bonini;J. Struct. Geol.,2007
5. Estimating uncertainties in 3-D models of complex fold-and-thrust belts: a case study of the Eastern Alps triangle zone;Brisson;Appl. Comput. Geosci.,2023
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