Flanking structure and single layer fold development in isotropic and anisotropic rock
Por um escritor misterioso
Last updated 08 junho 2024
Flanking structures around planar discontinuities in an otherwise homogeneous ow develop a characteristic geometry that is potentially a source of kinematic information about the background ow. Analytical methods were used to calculate the velocity around a thin weak inclusion (representing a fracture) in linear viscous material. This approach allows modelling of anking structures to very large strains. The velocity eld around a given anking structure can be calculated for the complete range of potential background ow elds, provided that the orientation of the fabric attractor and the bulk shear sense are known. Structures can be undeformed according to these velocity elds and, by quantifying the mis t between the actual and initial geometry, the vorticity number of the ow eld and the duration of deformation accurately determined. With these two parameters established, the background (bulk) deformation involved in the formation of a speci c anking structure can be calculated. This chapter was published in Journal of Structural Geology (Kocher and Mancktelow, 2005)
Transtensional flanking structures - ScienceDirect
PDF) Shear zone-related folds
Flanking structure and single layer fold development in isotropic and anisotropic rock
Comparison between input synthetic and output models for anisotropic
a) The strain distribution within a buckle formed in a homogeneous
Structural petrology
Flanking structure and single layer fold development in isotropic and anisotropic rock
Arka Debnath-M.Sc. Thesis by Arka's Digital Studio - Issuu
Deciphering the presence of axial-planar veins in tectonites - ScienceDirect
The role of preexisting anisotropy in structural styles of rifts and passive margins (Chapter 6) - Rifts and Passive Margins
Fault damage zones in mechanically layered rocks: The effects of planar anisotropy - Misra - 2015 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Re-folded structure of syn-orogenic granitoids (Padrón dome, NW Iberia): Assessing rheological evolution of cooling continental crust in a collisional setting - ScienceDirect
Flanking structure and single layer fold development in isotropic and anisotropic rock
Structures and Deformation in Glaciers and Ice Sheets - Jennings - 2021 - Reviews of Geophysics - Wiley Online Library
Deciphering the presence of axial-planar veins in tectonites - ScienceDirect
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