Area of Interest:

Earth Science and Geography

100%

Structural Geology

62%

Geography

90%

Himalayan Geology

75%

Geological Quarterly

55%

Research Publications in Numbers

Books
0

Chapters
0

Articles
0

Abstracts
0

Selected Publications

Mukherjee, S., C. Talbot and H.A. Koyi, 2010. Viscosity estimates of salt in the Hormuz and Namakdan salt diapirs, Persian Gulf. Geol. Mag., 147: 497-507.
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Mukherjee, S., 2010. Structures in meso- and micro-scales in the sutlej section of the higher himalayan shear zone, Indian himalaya. e-Terra, 7: 1-27.
Direct Link |
Mukherjee, S., 2010. Mineral fish: Their morphological classification, usefulness as shear sense indicators and genesis. Int. J. Earth Sci., 10.1007/s00531-010-0535-0.
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Mukherjee, S., 2010. Microstructures of the zanskar shear zone. Earth Sci. India, 3: 9-27.
Direct Link |
Mukherjee, S. and H.A. Koyi, 2010. 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.
CrossRef | Direct Link |
Mukherjee, S. and H.A. Koyi, 2009. 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., 10.1007/s00531-009-0459-8.
CrossRef | Direct Link |
Mukherjee, S. and H.A. Koyi, 2009. Flanking microstructures. Geol. Magazine, 146: 517-526.
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Mukherjee, S. and R. Chakraborty, 2007. Pull-apart micro-structures and associated passive folds. Ann. Trans. Nordic Rheol. Soc., 15: 247-252.
Direct Link |
Mukherjee, S., 2005. Prerequisite studies for numerical flow modeling to locate safe drinking water wells in the zone of arsenic polluted groundwater in the Yamuna sub-basin, West Bengal, India. Nat. Arsenic Groundwater Occurrence Remediat. Manage., .
Direct Link |
Jain, A.K., R.M. Manickavasagam, S. Singh and S. Mukherjee, 2005. Himalayan collision zone: New perspectives�its tectonic evolution in a combined ductile shear zone and channel flow model. Himalayan Geol., 26: 1-18.
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