Rebecca Farrington | M@TE

2 posts tagged with “Rebecca Farrington”

Stress evolution of more buoyant arc-continent collision. This style of collision results in slab break-off

Stress evolution of more buoyant arc-continent collision. This style of collision results in slab break-off

The Role of Lithospheric-Deep Mantle Interactions on the Style and Stress Evolution of Arc-Continent Collision

Uploaded by: Andres Felipe Rodriguez Corcho

Uploaded: May 24, 2024

Software: Underworld2

Tags:

arc-collision buoyancy contrast gravitational collapse slab-anchoring slab-folding

Finite Element MPI Particle-in-cell Python

Our simulations produce catchment areas, river lengths, and volumes of deposited sediment that are consistent with the ranges observed in continental-scale deltas such as the Mississippi and Amazon rivers. (a) Example showing the outputs from the numerical simulation showing the elevation and bathymetry (top) and cumulative flexure (bottom). Model dimensions are 4500 km x 2000 km, with a vertical exaggeration of 100x. (b) Scatter plot of river length (top) and 405 shelf width (bottom) versus catchment area from river systems. Data is from Somme et al. (2009), Nyberg et al. (2018), Blum et al. (2013, 2017) and simulations presented in this study. Pal= Paleocene, Oli=Oligocene, PM= Paleo-Mississippi. (c) Example of synthetic stratigraphy from a simulation without (left) and with flexural compensation (right).

Our simulations produce catchment areas, river lengths, and volumes of deposited sediment that are consistent with the ranges observed in continental-scale deltas such as the Mississippi and Amazon rivers. (a) Example showing the outputs from the numerical simulation showing the elevation and bathymetry (top) and cumulative flexure (bottom). Model dimensions are 4500 km x 2000 km, with a vertical exaggeration of 100x. (b) Scatter plot of river length (top) and 405 shelf width (bottom) versus catchment area from river systems. Data is from Somme et al. (2009), Nyberg et al. (2018), Blum et al. (2013, 2017) and simulations presented in this study. Pal= Paleocene, Oli=Oligocene, PM= Paleo-Mississippi. (c) Example of synthetic stratigraphy from a simulation without (left) and with flexural compensation (right).

Flexural isostatic response of continental-scale deltas to climatically driven sea level changes

Uploaded by: Sara Polanco

Uploaded: May 24, 2024

Software: Badlands

Tags:

Deltaic depocenters Flexural isostasy Glacial isostatic adjustment (GIA)Stratigraphic record

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