Layer-parallel shortening and related structures in zones undergoing active regional horizontal extension

@article{engr2012LayerparallelSA,
  title={Layer-parallel shortening and related structures in zones undergoing active regional horizontal extension},
  author={A. M. Cel{\^a}l Şeng{\"o}r and E. Bozkurt},
  journal={International Journal of Earth Sciences},
  year={2012},
  volume={102},
  pages={101-119}
}
Folds and thrust faults formed by layer-parallel shortening coaxial with extensional structures such as normal dip-slip faults and ductile necking structures with orthorhombic fabric symmetry are usual, but little-recognised structures formed within normal dip-slip shear zones bounding rifts. They are generated because of the shear distribution in a zone of progressive deformation and may be later extended and disrupted depending on which part of the strain ellipsoid they may be located. We… Expand
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