Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 73
Seismic activity in the Himalaya is mainly associated with active faults and folds
trending normal or oblique to the Himalayan trend which leads to the
underthrusting of the blocks . The present study area forms a part of Frontal
Himalayan Zone ...
Seismic activity in the Himalaya is mainly associated with active faults and folds
trending normal or oblique to the Himalayan trend which leads to the
underthrusting of the blocks . The present study area forms a part of Frontal
Himalayan Zone ...
Page 220
The second step in preconditioning is the trend removal . If not corrected for , this
may lead to superposition of a triangular bias on the data points , which in turn
leads to erroneous estimation of powers at long periods and thus needs to be ...
The second step in preconditioning is the trend removal . If not corrected for , this
may lead to superposition of a triangular bias on the data points , which in turn
leads to erroneous estimation of powers at long periods and thus needs to be ...
Page 287
are not uncommon . Such a trend is parallel to the regional structural and tectonic
trend indicating an intimate relationship between the drainage systems , and
structural tectonic lineaments of the state . Intimate relationship between geologic
...
are not uncommon . Such a trend is parallel to the regional structural and tectonic
trend indicating an intimate relationship between the drainage systems , and
structural tectonic lineaments of the state . Intimate relationship between geologic
...
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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