Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 24
Description : Carapace elongate ovate in lateral outline ; dorsal margin arched ,
ventral straight meeting the anterior and posterior margins in rounded curves ,
anterior rounded , posterior narrowly rounded ; left valve larger than the right and
...
Description : Carapace elongate ovate in lateral outline ; dorsal margin arched ,
ventral straight meeting the anterior and posterior margins in rounded curves ,
anterior rounded , posterior narrowly rounded ; left valve larger than the right and
...
Page 43
Deformation at the northern margin of Tibet is dominated by left - lateral slip at 20
mm / a or more along the east - northeast trending Altyn Tagh fault . In addition ,
roughly north - south crustal shortening at a few mm / a occurs by thrust faulting ...
Deformation at the northern margin of Tibet is dominated by left - lateral slip at 20
mm / a or more along the east - northeast trending Altyn Tagh fault . In addition ,
roughly north - south crustal shortening at a few mm / a occurs by thrust faulting ...
Page 49
Deformation at the northern margin of Tibet is dominated by left - lateral slip at 20
mm / a or more along the east - northeast trending Altyn Tagh fault . In addition ,
roughly north - south crustal shortening at a few mm / a occurs by thrust faulting ...
Deformation at the northern margin of Tibet is dominated by left - lateral slip at 20
mm / a or more along the east - northeast trending Altyn Tagh fault . In addition ,
roughly north - south crustal shortening at a few mm / a occurs by thrust faulting ...
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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 |
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Common terms and phrases
active 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