Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 108
A major tributary Kalpa ganga joins Alaknanda in right side at Helang . The
dominant part of Alaknanda basin is occupied by quartzite and gneissic rocks ,
calcareous rocks , slates and provides avenues for geomorphic analysis , which
aids in ...
A major tributary Kalpa ganga joins Alaknanda in right side at Helang . The
dominant part of Alaknanda basin is occupied by quartzite and gneissic rocks ,
calcareous rocks , slates and provides avenues for geomorphic analysis , which
aids in ...
Page 111
R VE the uplift along the NW and NE oriented faults which suggests that
Crystallines and Lesser Himalayan rocks existing along Alaknanda valley were
uplifted by faulting . This uplifting was responsible for the development of NE -
SW ...
R VE the uplift along the NW and NE oriented faults which suggests that
Crystallines and Lesser Himalayan rocks existing along Alaknanda valley were
uplifted by faulting . This uplifting was responsible for the development of NE -
SW ...
Page 114
At Helong rivers Kalpa and Karamnasa join the Alaknanda at right angles
opposite to each other . The beds of both the channels have slopes of more then
25° in steps and their straight course indicates the fault line scarp . The entire
river area ...
At Helong rivers Kalpa and Karamnasa join the Alaknanda at right angles
opposite to each other . The beds of both the channels have slopes of more then
25° in steps and their straight course indicates the fault line scarp . The entire
river area ...
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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