Meeting application CTSP 2018-029: Difference between revisions
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|CSDMS meeting last name=Dubey | |CSDMS meeting last name=Dubey | ||
|CSDMS meeting affiliation=National Centre for Earth Science Studies, Ministry of Earth Science, Government of India | |CSDMS meeting affiliation=National Centre for Earth Science Studies, Ministry of Earth Science, Government of India | ||
|CSDMS meeting city=Thiruvananthapuram | |CSDMS meeting city=Thiruvananthapuram, Kerala | ||
|CSDMS meeting country=India | |CSDMS meeting country=India | ||
|CSDMS meeting email address=p.dubey48@gmail.com | |CSDMS meeting email address=p.dubey48@gmail.com | ||
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{{Meeting statement interest | {{Meeting statement interest | ||
|Meetingstatement_of_interest_submit=At present, I am working on the problem of the evolution of elevated passive continental margin like Western Ghats, India and understanding the process of metamorphism and evolution of metamorphic rocks etc., which are the areas of large scientific interest. The Western Ghats at the western margin of Peninsular India is made up of several regional provinces like Deccan Plateau (DP), Dharwar Craton (DC) and Southern Granulite Terrain (SGT) and also covers the southern province of peninsular India. These provinces are traversed by several shear zones separating the different crustal blocks and in the need of delineating the nature underneath the deep-seated structures. Therefore, | |Meetingstatement_of_interest_submit=At present, I am working on the problem of the evolution of elevated passive continental margin like Western Ghats, India and understanding the process of metamorphism and evolution of metamorphic rocks etc., which are the areas of large scientific interest. The Western Ghats at the western margin of Peninsular India is made up of several regional provinces like Deccan Plateau (DP), Dharwar Craton (DC) and Southern Granulite Terrain (SGT) and also covers the southern province of peninsular India. These provinces are traversed by several shear zones separating the different crustal blocks and in the need of delineating the nature underneath the deep-seated structures. Therefore, detail integrated study need to be carried out for a better understanding of the settings of such zones that are important for tracing the tectonic history and their characteristics. | ||
Hence, CTSP: Coupling of Tectonic and Surface Processes workshop is a golden opportunity to learn the tectonic and surface processes that affects the deformation as well as subsurface structures upto a great depth. | Hence, CTSP: Coupling of Tectonic and Surface Processes workshop is a golden opportunity to learn the tectonic and surface processes that affects the deformation as well as subsurface structures upto a great depth. It also provides me a foremost opportunity to start a long lasting personal relation with CSDMS community. I am happy to be a part of it. | ||
Thank you. | |||
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{{Meeting abstract yes no | {{Meeting abstract yes no | ||
|CSDMS meeting abstract submit=Yes | |CSDMS meeting abstract submit=Yes | ||
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