Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
From inside the book
Results 1-3 of 6
Page 203
The stress orientations during these deformational phases were approximately 90 ° apart . ... Compressive stresses carried the thrust sheets to enormous heights along the ramps against the earth's gravity . As these compressive stresses ...
The stress orientations during these deformational phases were approximately 90 ° apart . ... Compressive stresses carried the thrust sheets to enormous heights along the ramps against the earth's gravity . As these compressive stresses ...
Page 206
With the increase in the compression the axial planes of these early folds provided favourable sites for the eventual shearing which was inevitable as ... This event marks the zenith of the compressive stresses around mid - Miocene .
With the increase in the compression the axial planes of these early folds provided favourable sites for the eventual shearing which was inevitable as ... This event marks the zenith of the compressive stresses around mid - Miocene .
Page 206
With the increase in the compression the axial planes of these early folds provided favourable sites for the eventual shearing which was inevitable as ... This event marks the zenith of the compressive stresses around mid - Miocene .
With the increase in the compression the axial planes of these early folds provided favourable sites for the eventual shearing which was inevitable as ... This event marks the zenith of the compressive stresses around mid - Miocene .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Fold shape analysis in the vicinity of North Almora Thrust in District | 121 |
Simla group problem in HimalayaA critical review | 131 |
Geology of Kishanpur NagrotaBasantgarhGujru Nagrota Sector of Inner | 137 |
8 other sections not shown
Other editions - View all
Common terms and phrases
active analysis associated average axis beds belt blocks central Chevron Folds compressive stresses crustal deformation developed direction displacement earthquake east east-west eastern estimated et al evidence exposed extension fault field folds Formation formed Garhwal Geol Geology grains granite Group Himalaya Himalayan Geology India indicate Jammu Jour landslide lateral left-lateral limestone lineation Lower major margin measurements melange metamorphism Mineral mm/a Molnar movement Murree normal faulting northern observed occurred oceanic offset ophiolitic orientation phase plane plateau Pradesh present pressure quartz quartzite range References region reported represent result rocks roughly samples sandstones seismic sequence Shan shape shear shortening Simla Sine Waves Siwalik Slates slip solutions southern specimens strain strike-slip faulting structures suggest surface Table Tapponnier tectonic thrust thrust faulting Tibet trending types units Upper valley volcanics western zone