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Microflanking Structures & Their Rheological Significance
Department of Earth Sciences, Indian Institute of Technology Roorkee, Uttarakhand, India.
Uppsala University, Disciplinary Domain of Science and Technology, Earth Sciences, Department of Earth Sciences, Solid Earth Geology. (Hans Ramberg Tectonic Laboratory)
2007 (English)In: Annual Transactions - The Nordic Rheology Society, ISSN 1601-4057, Vol. 15, 243-245 p.Article in journal (Refereed) Published
Abstract [en]

We report flanking structures from micro-scales from sheared rocks in the Himalaya, and designate them as ‘microflanking structures’. Cleavages and grain boundaries of host minerals act as shear plains and also impart anisotropy during shearing event. Rheological possibilities, other than a weaker host within a stronger matrix, have been encountered.

Place, publisher, year, edition, pages
2007. Vol. 15, 243-245 p.
National Category
Earth and Related Environmental Sciences
Identifiers
URN: urn:nbn:se:uu:diva-11418OAI: oai:DiVA.org:uu-11418DiVA: diva2:39187
Available from: 2008-01-29 Created: 2008-01-29 Last updated: 2017-12-11Bibliographically approved

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Koyi, Hemin A.

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