SM
Santanu Misra
Indian Institute of Technology Kanpur, Victoria University of Wellington, Jadavpur University, GNS Science
0000-0002-2364-1965
About
I am a Full Professor in the Department of Earth Sciences at Indian Institute of Technology, Kanpur (IIT Kanpur). I lead the Experimental Rock Deformation Laboratory in IIT Kanpur. Along with my students, I try to understand the chemo-mechanical response of composite rock systems at various deformation conditions.
See more here: https://home.iitk.ac.in/~smisra/
Employment
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Indian Institute of Technology Kanpur Full Professor2022 - Present
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Indian Institute of Technology Kanpur Associate Professor2018 - 2022
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Indian Institute of Technology Kanpur Assistant Professor2015 - 2018
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Victoria University of Wellington Guest Lecturer2014 - 2015
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GNS Science Senior Scientist2013 - 2015
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ETH Zürich Lectuter2009 - 2009
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ETH Zürich SNSF Post-Doctoral Fellow2007 - 2009
Education
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Jadavpur University PhD
Projects & Funding
Projects & funding information is unavailable.
Publications (56)
- Mechanical behavior and pressure-dependent porosity evolution in porous sandstone and limestone using triaxial deformation tests Save
- Deformation of the Paleoproterozoic Lower Vindhyan Group in Central India: synsedimentary origin or associated with the Mesoproterozoic convergence between the Bundelkhand and Bastar Cratons? Save
- Nanopore Heterogeneity and Accessibility in Oil and Gas Bearing Cretaceous KG (Raghampuram) Shale, KG Basin, India: An Advanced Multi-analytical Study Save
- Laboratory Observation of Fluid Flow in Depleted Shale Gas Reservoir: Coupling Effect of Sorbing and Non-sorbing Gas on Stress, Slippage, Flow Regime in Anisotropic and Fractured Shales Save
- CALDERA: a scientific drilling concept to unravel Connections Among Life, geo-Dynamics and Eruptions in a Rifting Arc caldera, Okataina Volcanic Centre, Aotearoa New Zealand Save
- Frictional Control on Accelerating Creep During the Slow‐To‐Fast Transition of Rainfall‐Induced Catastrophic Landslides Save
- Insights Into the Micromechanics of Dehydration‐Induced Gypsum to γ‐Anhydrite Phase Transition From Instrumented Microindentation Experiments Save
- Understanding the mudcrack patterns: How layer thickness, grain size, and secondary layers affect their formation – A laboratory study Save
- A numerical investigation of fluid flow path evolution during cataclastic flow in reservoir rocks Save
- Reaction-diffusion modelling of petrological mixing mechanisms in the evolution of continental crusts Save