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S-C fabrics in HHC. (a) The sigmoidal S-surfaces are deflected near the C-surfaces in the garnet –kyanite schist near Hirgo. The angle between S and C is ~21°. The sense of shear is top-to-ESE. (b) Intensely sheared mylonitic granite near Pene. The late extensional C′ -plane also further deflects the S –surfaces. (c) The C -plane deflecting S-surface in quartz-biotite schist near Menchuka (d) The sub-horizontal C-planes making acute angle with S-surfaces near Yapik village. The sense of shear is top-to-ESE. (Locations: Hirgo: 28°30'53.3"N: 94°26'99.8"E; Yapik: 28°30'69.3"N: 94°28'54.2" E; Menchuka: 28°36'036" N: 94°07'853" E)

S-C fabrics in HHC. (a) The sigmoidal S-surfaces are deflected near the C... Available to Purchase

Published: 01 November 2020
Fig.5. S-C fabrics in HHC. (a) The sigmoidal S-surfaces are deflected near the C-surfaces in the garnet –kyanite schist near Hirgo. The angle between S and C is ~21°. The sense of shear is top-to-ESE. (b) Intensely sheared mylonitic granite near Pene. The late extensional C′ -plane also
Journal Article

Thrust Shear Sense and Shear Zone Fabrics in the Higher Himalaya, Siyom Valley, Eastern Arunachal Himalaya, India Available to Purchase

Tapos Kumar Goswami, Sukumar Baruah, Bashab Nandan Mahanta, Pranjit Kalita, Polash Bora
Published: 01 November 2020
Jour. Geol. Soc. India (2020) 96 (5): 447–457.
DOI: https://doi.org/10.1007/s12594-020-1582-1
...Fig.5. S-C fabrics in HHC. (a) The sigmoidal S-surfaces are deflected near the C-surfaces in the garnet –kyanite schist near Hirgo. The angle between S and C is ~21°. The sense of shear is top-to-ESE. (b) Intensely sheared mylonitic granite near Pene. The late extensional C′ -plane also...
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View PDF for article title, Thrust Shear Sense and Shear Zone Fabrics in the Higher Himalaya, Siyom Valley, Eastern Arunachal Himalaya, <span class="search-highlight">India</span>
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