Journal of Himalayan Geology, Volume 6Wada Institute of Himalayan Geology, 1995 - Geology |
From inside the book
Results 1-3 of 67
Page 21
The highly anisotropic volcanic rocks interstratified with arenaceous rocks of the
Banjar Formation are completely enclosed within a thick pile of arenaceous
sequence ( isotropic rocks ) . The prograde metamorphism produced greenschist
- to ...
The highly anisotropic volcanic rocks interstratified with arenaceous rocks of the
Banjar Formation are completely enclosed within a thick pile of arenaceous
sequence ( isotropic rocks ) . The prograde metamorphism produced greenschist
- to ...
Page 27
The presence of feldspar and rock fragments is the result straight to sutured
contact resembles ' stretched quartz ' of balance between the rate of
decomposition and the rate of derivation from metamorphic rocks ( Blatt , 1967 ) .
According ...
The presence of feldspar and rock fragments is the result straight to sutured
contact resembles ' stretched quartz ' of balance between the rate of
decomposition and the rate of derivation from metamorphic rocks ( Blatt , 1967 ) .
According ...
Page 64
The junction between the Lesser Himalaya and the Outer Himalaya is marked by
MBT which separates the Tertiary rocks (Siwaliks) from the pre-Tertiary rocks (
Krol-Tal and Infra-Krols). The Main Frontal Thrust is another important tectonic ...
The junction between the Lesser Himalaya and the Outer Himalaya is marked by
MBT which separates the Tertiary rocks (Siwaliks) from the pre-Tertiary rocks (
Krol-Tal and Infra-Krols). The Main Frontal Thrust is another important tectonic ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
START | 1 |
GET FILE NAME | 72 |
S MUKHOPADHYAYA K N KHATTRI R CHANDER Seismic Velocity and Related Elastic Parameters | 6 |
17 other sections not shown
Other editions - View all
Common terms and phrases
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