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By Soumyajit Mukherjee

Study of buildings linked to shear zones is an important point to appreciate the deformation mechanism linked to such zones. Shear zones were emphasised because it will bring about many most modern utilized reports comparable to radioactive waste disposal, groundwater move and so forth. For the sake of brevity, study papers can't exhibit all attainable version in constructions present in shear zones. The proposed e-book goals to provide a few of these buildings in nice info with beautiful color images. each one photo can have a finished caption.

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Location Greater Himalayan Crystallines from Sutlej section, Himachal Pradesh, India 40 2 Folds Fig. 17 A tight polyclinally folded quartz vein cuts across foliations of mylonitized gneiss/ migmatite. Since this fold is not bound by foliations, it is not to be considered an ‘intrafolial fold’, and therefore is not to be used as a shear sense indicator. Greater Himalayan Crystallines, Sutlej section, India. Reproduced from Fig. 15c of Mukherjee (2010) Fig. 18 Quartz-rich foliations at places show hook-fabric [see Wennberg (1996) for modeled—and Mukherjee and Koyi (2010b) for micro-scale examples].

Its tails merge with the primary shear C-planes (= gneissosity = mylonitic foliation = main foliation) of the mylonitized gneiss. Delta structures are observed rarely from meso- and micro-scales, and indicate usually a high strain (Passchier and Trouw 2005). 4d of Mukherjee (2013b) from where this figure is reproduced. Notice that (1) at top left of the delta structure, an asymmetric quartz pod demonstrate the same shear sense; (2) when the tails and the clast are of the same minerals and both define a delta geometry, it has been described as a ‘rolling structure’ (Driessche and Brun 1996).

Location Greater Himalayan Crystallines, Bhagirathi section, India Fig. 24 Right to the marker (pen), a rootless flame fold of quartz with axial trace parallel to the left dipping mylonitic foliation. The fold does not indicate any shear sense. However, a few sigmoid quartz pods interconnected by secondary synthetic ductile shear C0 planes indicate reliably a top-to-right (up) shear, at top right portion of the photo. From mylonitized gneiss/ migmatite of Greater Himalayan Crystallines, Sutlej section, India 44 2 Folds Fig.

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