Morphotectonics And River Style Framework OF The Betwa River Central India

Morphotectonics And River Style Framework OF The Betwa River Central India

dc.contributor.guide	Prakash Kuldeep
dc.coverage.spatial
dc.creator.researcher	Mohanty Tanuja
dc.date.accessioned	2019-01-25T06:12:24Z
dc.date.available	2019-01-25T06:12:24Z
dc.date.awarded
dc.date.completed	2017
dc.date.registered	1-9-2011
dc.description.abstract	The topographic modifications in spatial and temporal scales are best reflected newlineby the dynamic river systems and their pathways. The Marginal Gangetic Alluvial Plain newline(MGAP) constitutes the southern part of the Ganga Plain active foreland basin, formed newlinedue to flexing of the Indian lithosphere brought about by thrust fold loading of the newlineHimalayan orogen. The western part of the MGAP is drained by the Yamuna and its newlineright bank tributaries, such as the Chambal, the Betwa, the Ken and the Tons Rivers. A newlinelarge portion of these river basins is underlain by rocks of Archaean Proterozoic age newlineand Deccan Trap rocks of Cretaceous age which reflect the changes in topographic newlinesurfaces, caused by epeirogenic deformation in the area. newline
dc.description.note
dc.format.accompanyingmaterial	CD
dc.format.dimensions
dc.format.extent
dc.identifier.uri	http://hdl.handle.net/10603/226863
dc.language	English
dc.publisher.institution	Department of Geology
dc.publisher.place	Varanasi
dc.publisher.university	Banaras Hindu University
dc.relation
dc.rights	university
dc.source.university	University
dc.subject.keyword	Physical Sciences,Geosciences,Geology
dc.title	Morphotectonics And River Style Framework OF The Betwa River Central India
dc.title.alternative
dc.type.degree	Ph.D.