Basic concept of deformation and strain is described. Strain ellipse and reciprocal strain ellipse are then introduced as the interface between deformation and strain. Mohr's circle is explained as the magnificent tool to obtain axial ratio and direction of axis of strain using graph instead of calculation. Practical techniques in field are described to measure axial ratio and direction of axis of strain. Practical techniques are the methods that use the strain grid, glass shard and fossils. The famous R_f/φ technique is explained that the method is invented from applying the theory of superposition of homogeneous strain
In a finite deformation x = x(X), a particle initially at X is displaced to x. Fundamental to the de...
Most of the existing methods of strain analysis can estimate strain in a single form of distorted br...
A simple algorithm based on the transformation equations of homogeneous deformation allows applicati...
Basic concept of deformation and strain is described. Strain ellipse and reciprocal strain ellipse a...
The estimation of the strain ellipse from data consisting of longitudinal strains measured along dif...
The shapes of the strain ellipse in homogeneous strain fields can be determined by measuring the cha...
The least square strain technique that was developed by Hayashi (1994) and is based on the least squ...
Abstract: Finite strain technique was applied for Abt schist, sheared granitoids and volcanosediment...
I have proposed three techniques for three dimensional strain analysis, that is, the orthogonal aver...
The coaxial and non-coaxial superposition of tectonic (biaxial or plane) strain on compactional (uni...
A method of strain analysis is described which takes into account a possible competence difference b...
The digital image processing technique can be successfully used to quickly measure surface deformati...
One of the main aims in the field of structural geology is the identification and quantification of ...
Several methods exist for the determination of the finite strain ellipsoid from deformed pebble shap...
This site contains visualizations for stress and strain analysis. These visualizations allow the stu...
In a finite deformation x = x(X), a particle initially at X is displaced to x. Fundamental to the de...
Most of the existing methods of strain analysis can estimate strain in a single form of distorted br...
A simple algorithm based on the transformation equations of homogeneous deformation allows applicati...
Basic concept of deformation and strain is described. Strain ellipse and reciprocal strain ellipse a...
The estimation of the strain ellipse from data consisting of longitudinal strains measured along dif...
The shapes of the strain ellipse in homogeneous strain fields can be determined by measuring the cha...
The least square strain technique that was developed by Hayashi (1994) and is based on the least squ...
Abstract: Finite strain technique was applied for Abt schist, sheared granitoids and volcanosediment...
I have proposed three techniques for three dimensional strain analysis, that is, the orthogonal aver...
The coaxial and non-coaxial superposition of tectonic (biaxial or plane) strain on compactional (uni...
A method of strain analysis is described which takes into account a possible competence difference b...
The digital image processing technique can be successfully used to quickly measure surface deformati...
One of the main aims in the field of structural geology is the identification and quantification of ...
Several methods exist for the determination of the finite strain ellipsoid from deformed pebble shap...
This site contains visualizations for stress and strain analysis. These visualizations allow the stu...
In a finite deformation x = x(X), a particle initially at X is displaced to x. Fundamental to the de...
Most of the existing methods of strain analysis can estimate strain in a single form of distorted br...
A simple algorithm based on the transformation equations of homogeneous deformation allows applicati...