Flanking structure and single layer fold development in isotropic and anisotropic rock
Por um escritor misterioso
Last updated 15 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)
Flanking structure development in anisotropic viscous rock - ScienceDirect
Information from folds: A review - ScienceDirect
Crustal shortening at the Sierra Pie de Palo (Sierras Pampeanas, Argentina): near-surface basement folding and thrusting, Geological Magazine
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
Resolving the Core and the Surface of CdSe Quantum Dots and Nanoplatelets Using Dynamic Nuclear Polarization Enhanced PASS–PIETA NMR Spectroscopy
Flanking structure and single layer fold development in isotropic and anisotropic rock
Transtensional origin of multi-order cross-folds in a high-grade gneiss complex, southwestern Grenville Province: formation during post-peak gravitational collapse
Flanking structure and single layer fold development in isotropic and anisotropic rock
Folds and Folding
Flanking structure and single layer fold development in isotropic and anisotropic rock
Salt Stocks and Salt Walls (Chapter 5) - Salt Tectonics
The association of folds and fractures and the link between folding, fracturing and fluid flow during the evolution of a fold–thrust belt: a brief review
Transtensional flanking structures - ScienceDirect
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