A K VERMA
Articles written in Journal of Earth System Science
Volume 129 All articles Published: 17 October 2020 Article ID 0213 Research article
In ductile shear zones, the strain shown by the rocks depends much on the composition and shape of the mineral constituents. Under simple shear, quartz grains commonly reorient themselves in the direction of tectonic transport or flow. In ductile shear zones, quartz grains are elliptically stretched in the direction of mylonitic foliation to accommodate the imposed ductile strain. Our observations on the rocks of a crustal scale shear zone, the Main Central Thrust (MCT) of the Himalaya, however, reveal that at several places of the shear zone the quartz grains are polygonal and show planar boundaries. The fabric of rocks at such places is not compatible with that of the prevailing fabric of rocks, and can be described as strain insensitive fabric. Following the Panozzo (
$\bullet$ The general fabric of rocks of ductile MCT zone of Himalaya is dominated by elliptically deformed quartz grains.
$\bullet$ However locally the fabric, not compatible with prevailing ductile fabric, contains polygonal quartz grains with flat boundaries.
$\bullet$ Strain has been estimated for polygonal grains by digitizing their outlines and analysing data by computer software.
$\bullet$ Such grains show lower strains near MCT and higher strains away. This is reversely shown by elliptically deformed grains.
$\bullet$ This suggests that the quartz grains with polygonal shapes remained rather insensitive to ductile strain.
Volume 130, 2021
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