Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 137
... crucial importance . Such studies either remained confined to field
observations or could only be initiated during the past decade only . It is because
of the fact that the terminologies for the geoscientific studies of the thrust belts
were evolved ...
... crucial importance . Such studies either remained confined to field
observations or could only be initiated during the past decade only . It is because
of the fact that the terminologies for the geoscientific studies of the thrust belts
were evolved ...
Page 232
These studies could also image the different synclines and anticlines and also
the thrust zones caused by the compressional tectonic forces . A significant
finding in this region is the undulation in the deep crust , extending to more than
30 km .
These studies could also image the different synclines and anticlines and also
the thrust zones caused by the compressional tectonic forces . A significant
finding in this region is the undulation in the deep crust , extending to more than
30 km .
Page 355
It is generally noticed that the road alignments are not selected by doing the
proper studies . For example most of the roads constructed are without much
consideration of geology , geomorphology and geohydrological considerations .
It is generally noticed that the road alignments are not selected by doing the
proper studies . For example most of the roads constructed are without much
consideration of geology , geomorphology and geohydrological considerations .
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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