Journal of Himalayan Geology, Volume 6Wada Institute of Himalayan Geology, 1995 - Geology |
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The SS . directions tectonic stress field in the Indian subcontinent trend N - NNE
to NE in the central and western India ( Gowd et ... This monoclinal feature
reflects some kind of compressive forces acting in the area at the time of its
formation .
The SS . directions tectonic stress field in the Indian subcontinent trend N - NNE
to NE in the central and western India ( Gowd et ... This monoclinal feature
reflects some kind of compressive forces acting in the area at the time of its
formation .
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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