Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 238
The author recalls a traverse ( with Sh . G . Malhotra , Geologist , GSI ) taken
along the Sirapatheng river in the ... PHYSIOGRAPHY The Siang districts form a
wild mountainous area consisting of roaring rivers and rivulets , deep gorges ,
lofty ...
The author recalls a traverse ( with Sh . G . Malhotra , Geologist , GSI ) taken
along the Sirapatheng river in the ... PHYSIOGRAPHY The Siang districts form a
wild mountainous area consisting of roaring rivers and rivulets , deep gorges ,
lofty ...
Page 292
Majority of the streams have sharp turnings before joining the main stream / river
course , or otherwise , when they change their courses . The tributaries also join
the main course at relatively high angles . All these features probably indicate a ...
Majority of the streams have sharp turnings before joining the main stream / river
course , or otherwise , when they change their courses . The tributaries also join
the main course at relatively high angles . All these features probably indicate a ...
Page 296
In the same manner , the streams and rivers of the Yu - Khampat river system
may also be , to a great extent , controlled by the transverse to oblique fractures
produced during the IMR tectogenesis thereby causing to run across the thrust ...
In the same manner , the streams and rivers of the Yu - Khampat river system
may also be , to a great extent , controlled by the transverse to oblique fractures
produced during the IMR tectogenesis thereby causing to run across the thrust ...
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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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Common terms and phrases
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