Abstract—An algorithm has been developed which allows the flexural deflection of the lithosphere to be calculated under thrust loading and the geometry of the sedimentary infill in the adjacent foreland basin. To that purpose we have considered arbitrarily shaped thrust-load systems moving towards the foreland, and surface processes denudating the orogen and filling the basin. The regional compensation of topographic loads is based on the assumption that the lithosphere behaves as a thin plate with either homogeneous (elastic, viscoelastic) behavior or more realistic depth-dependent elastic–plastic rheology. When using heterogeneous rheology, the program calculates the flexural behavior as a function of crus-tal geometry and thermal regime ...
Más información: https://sites.google.com/site/daniggcc/software/taoContacto: Garcia-Castellanos, D....
The basin between orogenic belt and craton is called foreland basin. However, in a sense it has been...
Main geodynamic and tectonic mechanisms responsible for evolution of foreland basins and their sedim...
An algorithm has been developed which allows the flexural deflection of the lithosphere to be calcul...
This chapter reviews a number of key advances in quantitative understanding of foreland basins since...
The tectonic evolution of sedimentary basins is the intrinsic result of the interplay between lithos...
A two-dimensional mathematical model considering coupling between a deforming elasto-visco-plastic f...
Foreland basins form by lithospheric flexure under orogenic loading and are filled by surface transp...
In collisional foredeeps, rifted continental margins become buried by foreland sedimentary deposits ...
In this thesis a tectono-sedimentary forward model has been presented, devised to simulate sediment ...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Previous quantitative studies dealing with the origin of foreland basins have focused primarily eith...
The purpose of this study is to evaluate the formation and shape of the Himalayan Foreland Basin sys...
Many mountain ranges in regions of plate convergence are flanked by foreland sedimentary basins that...
Foreland basin stratigraphy can be considered as the result of three interacting processes: thrust d...
Más información: https://sites.google.com/site/daniggcc/software/taoContacto: Garcia-Castellanos, D....
The basin between orogenic belt and craton is called foreland basin. However, in a sense it has been...
Main geodynamic and tectonic mechanisms responsible for evolution of foreland basins and their sedim...
An algorithm has been developed which allows the flexural deflection of the lithosphere to be calcul...
This chapter reviews a number of key advances in quantitative understanding of foreland basins since...
The tectonic evolution of sedimentary basins is the intrinsic result of the interplay between lithos...
A two-dimensional mathematical model considering coupling between a deforming elasto-visco-plastic f...
Foreland basins form by lithospheric flexure under orogenic loading and are filled by surface transp...
In collisional foredeeps, rifted continental margins become buried by foreland sedimentary deposits ...
In this thesis a tectono-sedimentary forward model has been presented, devised to simulate sediment ...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Previous quantitative studies dealing with the origin of foreland basins have focused primarily eith...
The purpose of this study is to evaluate the formation and shape of the Himalayan Foreland Basin sys...
Many mountain ranges in regions of plate convergence are flanked by foreland sedimentary basins that...
Foreland basin stratigraphy can be considered as the result of three interacting processes: thrust d...
Más información: https://sites.google.com/site/daniggcc/software/taoContacto: Garcia-Castellanos, D....
The basin between orogenic belt and craton is called foreland basin. However, in a sense it has been...
Main geodynamic and tectonic mechanisms responsible for evolution of foreland basins and their sedim...