Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/127853
Title: The impact of syn- and post-extension prograding sedimentation on the development of salt-related rift basins and their inversion: Clues from analogue modelling
Author: Moragas Rodriguez, Mar
Vergés i Masip, Jaume
Nalpas, Thierry
Saura, Eduard
Martín, Juan Diego (Martín Martín)
Messager, Grégoire
William Hunt, David
Keywords: Sedimentació
Tectònica
Models geològics
Sedimentation and deposition
Tectonics
Geological modeling
Issue Date: 1-Dec-2017
Publisher: Elsevier B.V.
Abstract: Various studies have demonstrated the intrinsic interrelationship between tectonics and sedimentation in salt-related rift basins during extension as well as during their inversion by compression. Here, we present seven brittle-ductile analogue models to show that the longitudinal or transverse progradation of sediment filling an elongate extensional basin has a substantial impact on the growth of diapirs and their lateral geometrical variations. We use five extensional models to reveal how these prograding systems triggered diapir growth variations, from proximal to distal areas, relative to the sedimentary source. In the models, continuous passive diapir walls developed, after a short period of reactive-active diapiric activity, during syn-extensional homogeneous deposition. In contrast, non-rectilinear diapir walls grew during longitudinal prograding sedimentation. Both longitudinal and transverse post extensional progradation triggered well-developed passive diapirs in the proximal domains, whereas incipient reactive-active diapirs, incipient roller-like diapirs, or poorly developed diapirs were generated in the distal domains, depending on the modelled sedimentary pattern. Two models included final phases of 6% and 10% shortening associated with basin inversion by compression, respectively, to discriminate compressional from purely extensional geometries. With the applied shortening, the outward flanks of existing diapir walls steepened their dips from 8 degrees-17 degrees to 30 degrees-50 degrees. Likewise, 6% of shortening narrowed the diapir walls by 32%-72%, with their fully closing (salt welds) with 10% of shortening. We compare our results with the distribution of salt walls and minibasins of the Central High Atlas diapiric basin in Morocco, which was infilled with a longitudinally prograding mixed siliciclastic and carbonatic depositional sequence during the Early-Middle Jurassic with a minimum thicknesses of 2.5-4.0 km. (C) 2017 Elsevier Ltd. All rights reserved.
Note: Versió postprint del document publicat a: https://doi.org/10.1016/j.marpetgeo.2017.10.001
It is part of: Marine and Petroleum Geology, 2017, vol. 88, p. 985-1003
URI: http://hdl.handle.net/2445/127853
Related resource: https://doi.org/10.1016/j.marpetgeo.2017.10.001
ISSN: 0264-8172
Appears in Collections:Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

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