Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 56
MAGNETIC AND GRAVITY STUDIES Regional scale potential field anomalies of
the earth provide important constraints for defining basic model for plate tectonics
and intra - plate deformation . Lack of data on such a regional scale has ...
MAGNETIC AND GRAVITY STUDIES Regional scale potential field anomalies of
the earth provide important constraints for defining basic model for plate tectonics
and intra - plate deformation . Lack of data on such a regional scale has ...
Page 259
The Kashmir Valley ( 74-75 ° E , 34.0-35 ° N ) , the Chamba region ( 32.50-33.5 °
N , 75.50-76.5 ° E ) and the Kinnaur region ( 31.5-33.0 ° N , 78-79 ° E ) are
characterized by appreciable seismicity . As explained by Ni and Barazang (
1984 ) ...
The Kashmir Valley ( 74-75 ° E , 34.0-35 ° N ) , the Chamba region ( 32.50-33.5 °
N , 75.50-76.5 ° E ) and the Kinnaur region ( 31.5-33.0 ° N , 78-79 ° E ) are
characterized by appreciable seismicity . As explained by Ni and Barazang (
1984 ) ...
Page 262
Central Himalaya Region This region mostly includes the Nepalese Himalaya
extending from 80 ° to 88 ° E , 26.5 ° to 31 ° N . This is one of the most active
regions of the Himalaya . Seismicity in this region has been discussed in detail by
...
Central Himalaya Region This region mostly includes the Nepalese Himalaya
extending from 80 ° to 88 ° E , 26.5 ° to 31 ° N . This is one of the most active
regions of the Himalaya . Seismicity in this region has been discussed in detail by
...
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Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
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Common terms and phrases
active Asia associated base basement basic basin beds belt biotite blocks Boundary Central collision complex consists continental continuous Cretaceous crust crystalline deformation deposits direction early earthquakes east eastern Eocene et al evolution extension facies faults Figure folds followed formation formed Gansser Garhwal Geol Geology gneiss grade granite Group Higher Himalaya Indian Indian plate indicate Indus initial island Jour Kashmir Ladakh Late Lesser levels limestone Lower magmatic major margin metamorphism Middle mountain movement nappe nature Nepal northern observed occur oceanic ophiolite origin orogenic Pakistan palaeomagnetic Palaeozoic Pande phase plate possible Precambrian present Range region represent rocks rotation sampled sandstones schists sedimentary sediments seismicity sequence Shield similar southern structural studies subduction suggested suture Table tectonic Tertiary Tethyan thickness thrust Tibetan trend units Upper valley volcanics western zone