Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 36
These residual deposits have been placed under the Skinding Formation ... are
overlain by conglomerate containing pebbles and cobbles of granitoids as well
as of red sandstone and gritty sandstone representing the residual deposits .
These residual deposits have been placed under the Skinding Formation ... are
overlain by conglomerate containing pebbles and cobbles of granitoids as well
as of red sandstone and gritty sandstone representing the residual deposits .
Page 43
of residual deposits ( Skinding Formation ) prior to deposition of the Miocene
Kargil Member . The provenance of the sediments was mainly from the northerly
Ladakh Granitoids during deposition of the Kargil and the overlying Tharumsa ...
of residual deposits ( Skinding Formation ) prior to deposition of the Miocene
Kargil Member . The provenance of the sediments was mainly from the northerly
Ladakh Granitoids during deposition of the Kargil and the overlying Tharumsa ...
Page 114
The fill deposits and the Pleistocene terraces are found along the valley on the
Alaknanda up to Pandukeshwar where terminal moraines are present ( Shah ,
1991 ) . In Badrinathji right side slope is gentle towards the Alaknanda . On the
left ...
The fill deposits and the Pleistocene terraces are found along the valley on the
Alaknanda up to Pandukeshwar where terminal moraines are present ( Shah ,
1991 ) . In Badrinathji right side slope is gentle towards the Alaknanda . On the
left ...
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Contents
Evidence | 1 |
Tectonomagmatic Evolutionary Model of the KuluRampur | 47 |
Tectonic and Geochemical Signifcance of Black Shale | 65 |
Copyright | |
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active Alaknanda Arunachal associated bands basin beds belt biotite Central characterized concentration Crystalline deformation Delhi deposits developed direction drainage Early east eastern elements et al evidence exposed extending fault field Figure folds Formation fractures further Garhwal Geol Geological Glacial glacier gneisses grains granite granitoids Group Himalaya India indicate Indus Kuhle Ladakh Late length Lesser limestone lineaments Lower Main major margin metamorphic moraines mountain nature ND ND normal northern Nummulitic observed occur Pakistan parallel pattern phyllites places plane plate Pleistocene Pradesh present quartzite range region represented resulted river rocks Saklani samples schist sediments sequence shale Siang districts side similar Siyom slide slope southern streams structural studies suggest surface Suture Table tectonic thick thrust Tibet trend unit upper valley values Volcanics western zone