2018
DOI: 10.1016/j.tecto.2018.08.012
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Formation and inversion of salt-detached ramp-syncline basins. Results from analog modeling and application to the Columbrets Basin (Western Mediterranean)

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Cited by 32 publications
(35 citation statements)
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“…That means that the buoyancy of the ductile layer in the model is larger than that in the natural cases. This limitation is common in sand-silicone analog experiments, and it has been shown that it does not affect firstorder model results (e.g., Bonini, 2001;Bahroudi and Koyi, 2003;Ferrer et al, 2016;Roma et al, 2018). For the viscous layer, we used the Hormuz evaporites as reference, with a viscosity range from 10 18 to 10 21 Pa s (Mukherjee et al, 2010;Sadeghi et al, 2016; Table 1).…”
Section: Scalingmentioning
confidence: 99%
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“…That means that the buoyancy of the ductile layer in the model is larger than that in the natural cases. This limitation is common in sand-silicone analog experiments, and it has been shown that it does not affect firstorder model results (e.g., Bonini, 2001;Bahroudi and Koyi, 2003;Ferrer et al, 2016;Roma et al, 2018). For the viscous layer, we used the Hormuz evaporites as reference, with a viscosity range from 10 18 to 10 21 Pa s (Mukherjee et al, 2010;Sadeghi et al, 2016; Table 1).…”
Section: Scalingmentioning
confidence: 99%
“…Finally, it must be stressed that in our models, the buoyancy of the ductile layer is higher than in the natural cases (Table 1), which should have some influence on the experiment dynamics. Nevertheless, this behavior is assumed in most of the analog modeling set for the simulation of deformation in upper crustal levels (see models of Ferrer et al, 2016;Li and Mitra, 2017;Borderie et al, 2018;Roma et al, 2018 who used the same analog materials as in this paper). Moreover, at the beginning of our experiments, the lateral flow of the silicone was limited, as it was confined by sand.…”
Section: Initial Sand-silicone Packmentioning
confidence: 99%
“…This fact implies high uncertainty and low confidence in the position and geometry of the horizons in the structural model built based on the picking of reflectors (Leahy and Skorstad, 2013). The poor quality of seismic data near faults also generate high uncertainty in their interpretation (Thore et al, 2002;Røe et al, 2014). Generally, faults do not generate seismic reflections, and they are interpreted based on reflector terminations.…”
Section: Introductionmentioning
confidence: 99%
“…Nevertheless, reflector terminations can also be produced by other geophysical and geological factors, such as noise in the seismic data, stratigraphic pinchouts, facies changes or unconformities (Alcalde et al, 2017b). Additionally, faults are typically interpreted as singular surfaces whereas they are zones of deformation (Røe et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
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