Parasitic folds represent a common structure of multi-scale multilayer folds and the resulting asymmetric S- or Z-shapes and symmetric M-shapes represent a complex strain distribution. How the strain evolution affects the resulting porosity remains unclear. In this study, a 2-D plane strain finite element modeling approach is used to simulate multi-scale, multilayer, viscoelastic buckle folds under in-situ stress and pore pressure conditions. A variety of material and model parameters (including the elastic modulus contrast, number of layers, viscosity contrast, strain rate and layer thickness ratio) are considered and their influence on the shape of parasitic folds and on the resulting porosity distribution is analyzed. This study demonstr...
Non-cylindrical sheath folds often develop by the accentuation of inherent geometrical irregularitie...
Sheath folds are highly non-cylindrical folds occurring in a variety of geological settings, and hav...
We analyze folding phenomena in finely layered viscoelastic rock. Fine is meant in the sense that th...
Over the past several decades, buckle folds have been exclusively studied by numerous methods. Howev...
Pore pressure and fluid flow during the deformational history of geologic structures are directly in...
Buckle folds of single-layer and multilayer sedimentary strata characterized are among the most comm...
Buckle folds of sedimentary strata commonly feature a variety of different fracture sets. Some fract...
Tensile failure associated with buckle folding is commonly associated to the distribution of outer a...
Subsurface engineering applications such as waste water disposal or CO2 sequestration require the se...
International audienceA model for finely layered visco-elastic rock proposed by us in previous paper...
Neutral surface folding is a significant contributor to fold development. This mechanism produces co...
This study extends the analytical solution of folding from a single-layer system to a multi-layer sy...
A continuous variation in fold style from chevron to very rounded profiles can be generated in an in...
A model for finely layered visco-elastic rock proposed by us in previous papers is revisited and gen...
AbstractIn this work, we propose a constitutive model for the finite-strain, macroscopic response of...
Non-cylindrical sheath folds often develop by the accentuation of inherent geometrical irregularitie...
Sheath folds are highly non-cylindrical folds occurring in a variety of geological settings, and hav...
We analyze folding phenomena in finely layered viscoelastic rock. Fine is meant in the sense that th...
Over the past several decades, buckle folds have been exclusively studied by numerous methods. Howev...
Pore pressure and fluid flow during the deformational history of geologic structures are directly in...
Buckle folds of single-layer and multilayer sedimentary strata characterized are among the most comm...
Buckle folds of sedimentary strata commonly feature a variety of different fracture sets. Some fract...
Tensile failure associated with buckle folding is commonly associated to the distribution of outer a...
Subsurface engineering applications such as waste water disposal or CO2 sequestration require the se...
International audienceA model for finely layered visco-elastic rock proposed by us in previous paper...
Neutral surface folding is a significant contributor to fold development. This mechanism produces co...
This study extends the analytical solution of folding from a single-layer system to a multi-layer sy...
A continuous variation in fold style from chevron to very rounded profiles can be generated in an in...
A model for finely layered visco-elastic rock proposed by us in previous papers is revisited and gen...
AbstractIn this work, we propose a constitutive model for the finite-strain, macroscopic response of...
Non-cylindrical sheath folds often develop by the accentuation of inherent geometrical irregularitie...
Sheath folds are highly non-cylindrical folds occurring in a variety of geological settings, and hav...
We analyze folding phenomena in finely layered viscoelastic rock. Fine is meant in the sense that th...