Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 1
Furthermore , lithological units involved along these two sections are sufficiently
different to suggest that the traditional image of a cylindrical Himalayan Belt is not
valid beyond the Karakoram Fault . A structural sketch upgraded in the light of ...
Furthermore , lithological units involved along these two sections are sufficiently
different to suggest that the traditional image of a cylindrical Himalayan Belt is not
valid beyond the Karakoram Fault . A structural sketch upgraded in the light of ...
Page 75
Himalayan Belt in the north and the Frontal Folded Belt in the south ( Kumar et al
1989 ) . These two are separated by the MBT . The Frontal Folded Belt essentially
consists of Sabathus , Dharamsalas , Siwaliks and recent sediments , whereas ...
Himalayan Belt in the north and the Frontal Folded Belt in the south ( Kumar et al
1989 ) . These two are separated by the MBT . The Frontal Folded Belt essentially
consists of Sabathus , Dharamsalas , Siwaliks and recent sediments , whereas ...
Page 243
Each litho - package constitutes a distinct and well defined tectonic belt and
altogether seven belts have been demarcated . From south to north , these belts
are - ( 1 ) Siwalik Belt , ( 2 ) Gondwana Belt , ( 3 ) Dedza - Menga Belt , ( 4 )
Bomdila ...
Each litho - package constitutes a distinct and well defined tectonic belt and
altogether seven belts have been demarcated . From south to north , these belts
are - ( 1 ) Siwalik Belt , ( 2 ) Gondwana Belt , ( 3 ) Dedza - Menga Belt , ( 4 )
Bomdila ...
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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