Titlebook: Quaternary Geomorphology in India; Case Studies from th Balai Chandra Das,Sandipan Ghosh,Aznarul Islam Book 2019 Springer International Pub

lipids

同步左右

Modes of Formation, Palaeogene to Early Quaternary Palaeogenesis and Geochronology of Laterites in part of India) which are found as distinct badland terrain and litho-stratigraphic unit, developed in between the eastern fringe of Chotanagpur Plateau (Rajmahal Basalt Traps, Gondwana sedimentary and Archaean rocks) and the western fringe of Bengal Basin (Rarh Bengal). These laterites are analyzed

Jogging

,Microstructural Evidence of Palaeo-Coastal Landform from Westernmost Fringe of Lower Ganga–Brahmapu westernmost fringe of this G-B delta has long been influenced by both Chottonagpur upland as well as recent alluvium plain between the Cretaceous to early Quaternary period. Successively, the undulating Rarh topography that separates these two morphogenic units has been evolved as one of the relict

CHARM

Influence of Faulting on the Extra-Channel Geomorphology of the Ajay-Damodar Interfluve in Lower Gad field investigation. In corresponding to the in-stream deformation, extra-stream area is also modified with extended swampy floodplain, unpaired terraces, large alluvial fans, and palaeochannels. Floodplain becomes waterlogged or swampy especially downstream section across the stream fault line. S

魅力

Geophysical Control on the Channel Pattern Adjustment in the Kunur River Basin of Western Part of Lttern adjustment. Over the Western Bengal Basin (WBB), EW-tending and NS-tending garbens are actively controlled the gravity anomaly and adjacent variation in basement structure and lithology. The streamlines of Kunur River Basin (KRB) and rivers in surrounding are sharply controlled by the variatio

AORTA

Imprints of Neo-tectonism in the Evolutionary Record Along the Course of Khari River in Damodar Fanarly portrayed the imprints of neo-tectonism in the forms of rapidly changing meander geometry, deformation in long profiles, unpaired terraces, soft sediment structures (fluid escape structure and convolute), etc. The study of meander geometry considering 142 loops (upper—92, middle—38 and lower—12

Infant

Historical Evidences in the Identification of Palaeochannels of Damodar River in Western Ganga-Brah Among many approaches, at the primary level, the written evidences like old literatures may be used as basic tools for palaeochannel identification and mapping. India being rich in religious texts and literatures, offers a vast scope for the study of historical geography as well as palaeo-geography

Graves’-disease

未成熟

SLAG