Atlas of Shear Zone Structures in Meso-scale by Soumyajit Mukherjee

By Soumyajit Mukherjee

Study of buildings linked to shear zones is an important element to appreciate the deformation mechanism linked to such zones. Shear zones were emphasised because it will result in many most recent utilized stories similar to radioactive waste disposal, groundwater circulation and so on. For the sake of brevity, examine papers can't exhibit all attainable edition in buildings present in shear zones. The proposed publication goals to offer a few of these buildings in nice info with appealing color images. every one photo may have a finished caption.

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Tuebingen University, Germany Mukherjee S, Koyi HA (2010a) 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 99:1267–1303 Mukherjee S, Koyi HA (2010b) 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 99:1083–1110 Mukherjee S, Punekar JN, Mahadani T et al (2013) Intrafolial folds—review and examples from the western Indian Higher Himalaya.

Being symmetric, no ductile shear sense is indicated. Location: Greater Himalayan Crystallines, Bhagirathi section, India. See Mukherjee (2013b) for a latest review on tectonics of this terrain 3 Veins and Near Symmetric Clasts 53 Fig. 3 A symmetric rhombic u-structure defined by an aggregate of quartzofeldspathic minerals. No shear sense indicated. From mylonitized gneiss at Bhagirathi section of Greater Himalayan Crystallines, India Fig. 4 Irregular feldspar clasts—a few rhombic, do not indicate any shear sense.

Symmetric objects in ductile shear zones that do not decode shear sense has been exemplified under optical microscopes by many such as Passchier and Trouw (2005) and Mukherjee (2013a). Most of the photographs described in this section for symmetric clasts and unshared veins bear no tectonic connotations. S. 1007/978-3-319-00089-3_3, Ó Springer International Publishing Switzerland 2014 51 52 3 Veins and Near Symmetric Clasts Fig. 1 A near-symmetric rhombic bulged part of a quartz vein. No clear ductile shear sense indicated.

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