Journal of Himalayan Geology, Volume 6Wada Institute of Himalayan Geology, 1995 - Geology |
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Page 1
To its south lies a complementary fold structure , Mohand anticline , and to its
north is the Satokgarh anticline . These fold structures have folded the Siwalik
strata and owe their origin as fault - propogation folds developed as a result of ...
To its south lies a complementary fold structure , Mohand anticline , and to its
north is the Satokgarh anticline . These fold structures have folded the Siwalik
strata and owe their origin as fault - propogation folds developed as a result of ...
Page 6
The Mohand anticline , the Dun syncline and the Santokgarh anticline were
developed as fault - propogated folds ... was also initiated around that time i.e.
500,000 years B.P. Mohand anticline is interpreted as fault - propogated fold (
Suppe ...
The Mohand anticline , the Dun syncline and the Santokgarh anticline were
developed as fault - propogated folds ... was also initiated around that time i.e.
500,000 years B.P. Mohand anticline is interpreted as fault - propogated fold (
Suppe ...
Page 7
Dun Syncline Fig . 6.Schematic interpretation for tectonic evolution of Dun Valley
showing fault ( HFT ) , propogated folds ( Mohand anticline , Dun syncline and
Santokhgarh anticline ) and tectonically controlled drainage ( arrows ) .
Dun Syncline Fig . 6.Schematic interpretation for tectonic evolution of Dun Valley
showing fault ( HFT ) , propogated folds ( Mohand anticline , Dun syncline and
Santokhgarh anticline ) and tectonically controlled drainage ( arrows ) .
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Contents
START | 1 |
GET FILE NAME | 72 |
S MUKHOPADHYAYA K N KHATTRI R CHANDER Seismic Velocity and Related Elastic Parameters | 6 |
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activities average beds block boundary carried caused changes climatic conservation cover deciduous degraded Dehra Dun Delhi deposits depth distribution dominant Doon Valley earthquake effect elements environment environmental erosion fault flow forest formation Ganga Garhwal given gravels ground growth Gujjars higher hills Himalayan Geology houses human important increase India indicate Institute Jour Lamayuru land lichen limestone located lower major measures minerals mining mixed moist Mussoorie natural northern observed occur park period Plan plants pollution population present production protection radon Rajaji range References region reported result river rocks samples sandstone scale sediments Shorea robusta shows Siwalik slopes soil species springs streams structure surface Table tectonic Thrust trees types units uplift upper various vegetation villages Yamuna zone