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

By Soumyajit Mukherjee

ISBN-10: 3319000888

ISBN-13: 9783319000886

ISBN-10: 3319000896

ISBN-13: 9783319000893

Study of constructions linked to shear zones is a vital element to appreciate the deformation mechanism linked to such zones. Shear zones were emphasised because it will result in many most modern utilized reports resembling radioactive waste disposal, groundwater move and so forth. For the sake of brevity, examine papers can't express all attainable edition in constructions present in shear zones. The proposed booklet goals to provide a few of these buildings in nice information with beautiful color images. each one picture may have a accomplished caption.

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Extra info for Atlas of Shear Zone Structures in Meso-scale

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Location: Greater Himalayan Crystallines, Bhagirathi section, India 56 3 Veins and Near Symmetric Clasts Fig. 9 Irregular feldspar clasts, do not indicate any shear sense. Location: Greater Himalayan Crystallines, Bhagirathi section, India Fig. 10 Elongated clast of quartz parallel to the main foliation. No shear sense indicated. Location: Greater Himalayan Crystallines, Bhagirathi section, India 3 Veins and Near Symmetric Clasts 57 Fig. 11 Inside anastomosed foliated ductile sheared rock, symmetric clasts of rather irregular shapes persist.

Near Karcham, Greater Himalayan Crystallines, Sutlej section, Himachal Pradesh, India 38 2 Folds Fig. 13 Top-to-right (up) ductile sheared migmatitic foliations. At places brittle rupture in the same shear sense took place. Greater Himalayan Crystallines, Sutlej section, Himachal Pradesh, India. Reproduced from Fig. 15d in Mukherjee (2010) Fig. 14 Overturned intrafolial fold of quartz vein. Top-to-right (up) sheared. Pronounced shear led to boudinage. From mylonitized gneiss/migmatite of Greater Himalayan Crystallines, Sutlej section, India 2 Folds 39 Fig.

51 A basalt flow layer consisting of curved sheared elongated zeolite vesicles. Comparing these sheared vesicles with S-fabric’s curvature, we can assign a top-to-left shear. However, this deformation is most likely to be due to lava flow and is not related to tectonics. Deccan trap basalt at Malsejghat, Maharashtra Fig. 52 ‘Arrow-head’ zeolite vesicles from the Deccan trap basalt at Malsejghat. Maharashtra. Curved internally strained individual zeolite vesicles define limbs of individual arrows.

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

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