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Please use this identifier to cite or link to this item: http://dspace.library.iitb.ac.in/jspui/handle/10054/5808

Title: Evidence of ductile shearing from the extensional crenulation cleavage: An example from Zawar area, the Aravalli mountain
Authors: BISWAL, TK
NAYAK, S
HARISH, TR
UNIKRISHNAN, S
Keywords: anisotropic rocks
zone
Issue Date: 1997
Publisher: CURRENT SCIENCE ASSN
Citation: CURRENT SCIENCE, 73(8), 701-703
Abstract: Extensional crenulation cleavage marked by asymmetric kinks and ductile shears occurs at low angle to steep S-1 planes in the mica schist of Zawar area in the Aravalli mountain. It is developed due to extension along the S-1 planes consequent to large-scale ductile shearing. The compressive stress of such shearing is deduced to be subhorizontal in NNE-SSW direction. Early fold axes assume variable trend due to shearing.
URI: http://dspace.library.iitb.ac.in/xmlui/handle/10054/5808
http://hdl.handle.net/10054/5808
ISSN: 0011-3891
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