General shear extrusion can thus account for both ductile non-coaxial deformation and inverted isograds, without requiring inverted isotherms at peak.
The studies presented above show that fabrics both at the northern contact of the batholith and inside the batholith formed during oblate coaxial deformation.
Mineral lineations and kinematic indicators in the country rock imply non-coaxial strain with a shear direction similar to that inferred for the shear zone.
Coaxial helices form when nucleobases from two separate helices stack, forming a pseudocontinuous helix.
Numerical study of coaxial double z-pinch for resonant photopumping x-ray laser.
In the transformer with such a coaxial structure, the cross-section area for the inner magnetic core is smaller than that of the outer magnetic core.
Large scale folding during distributed shear is regarded as a fundamental part of non-coaxial deformation.
All of this indicates that the perfect three-way junction does not generally fold by pairwise coaxial stacking of helices.
