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2013 | OriginalPaper | Buchkapitel

4. Intrafolial and Other Folds in Shear Zones

verfasst von : Soumyajit Mukherjee

Erschienen in: Deformation Microstructures in Rocks

Verlag: Springer Berlin Heidelberg

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Abstract

Intrafolial folds are tight to isoclinal syn-shear overturned folds in ductile shear zones. These folds could be bound by both primary–and secondary ductile shear planes.

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Literatur
Zurück zum Zitat Mukherjee S (2001) Shear sense reversal (SSR): definition, Classification and geodynamics implication with special reference to NW Himalaya. M.Tech seminar Report, Department of Earth Sciences, University of Roorkee, pp 1–31 Mukherjee S (2001) Shear sense reversal (SSR): definition, Classification and geodynamics implication with special reference to NW Himalaya. M.Tech seminar Report, Department of Earth Sciences, University of Roorkee, pp 1–31
Zurück zum Zitat Mukherjee S (2010a) Structures at Meso–and Micro-scales in the Sutlej section of the Higher Himalayan Shear Zone in Himalaya. e-Terra 7, 1–27 Mukherjee S (2010a) Structures at Meso–and Micro-scales in the Sutlej section of the Higher Himalayan Shear Zone in Himalaya. e-Terra 7, 1–27
Zurück zum Zitat Mukherjee S (2010b) Microstructures of the Zanskar Shear Zone. Earth Sci India 3:9–27 Mukherjee S (2010b) Microstructures of the Zanskar Shear Zone. Earth Sci India 3:9–27
Zurück zum Zitat Mukherjee S (2012) A polyclinally folded biotite grain in micro-scale. Int J Earth Sci 101:1009CrossRef Mukherjee S (2012) A polyclinally folded biotite grain in micro-scale. Int J Earth Sci 101:1009CrossRef
Zurück zum Zitat Mukherjee S, Koyi HA (2010a) Higher Himalayan Shear Zone, Zanskar Indian Himalaya—microstructural studies and extrusion mechanism by a combination of simple shear and channel flow. Int J Earth Sci 99:1083–1110CrossRef Mukherjee S, Koyi HA (2010a) Higher Himalayan Shear Zone, Zanskar Indian Himalaya—microstructural studies and extrusion mechanism by a combination of simple shear and channel flow. Int J Earth Sci 99:1083–1110CrossRef
Zurück zum Zitat Mukherjee S, Koyi HA (2010b) Higher Himalayan Shear Zone, Sutlej section: structural geology and extrusion mechanism by various combinations of simple shear, pure shear and channel flow in shifting modes. Int J Earth Sci 99:1267–1303CrossRef Mukherjee S, Koyi HA (2010b) Higher Himalayan Shear Zone, Sutlej section: structural geology and extrusion mechanism by various combinations of simple shear, pure shear and channel flow in shifting modes. Int J Earth Sci 99:1267–1303CrossRef
Zurück zum Zitat Mukherjee S, Punekar JN, Mahadani T, Mukherjee R (submitted) Intrafolial folds- review & examples from the western Indian Higher Himalaya. J Geosci Mukherjee S, Punekar JN, Mahadani T, Mukherjee R (submitted) Intrafolial folds- review & examples from the western Indian Higher Himalaya. J Geosci
Zurück zum Zitat Wennberg OP (1996) Superimposed fabric due to reversal of shear sense: an example from the Bergen Arc Shear Zone, western Norway. J Struct Geol 18:871–889CrossRef Wennberg OP (1996) Superimposed fabric due to reversal of shear sense: an example from the Bergen Arc Shear Zone, western Norway. J Struct Geol 18:871–889CrossRef
Metadaten
Titel
Intrafolial and Other Folds in Shear Zones
verfasst von
Soumyajit Mukherjee
Copyright-Jahr
2013
Verlag
Springer Berlin Heidelberg
DOI
https://doi.org/10.1007/978-3-642-25608-0_4