Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 44
the Altyn Tagh, the Kunlun and the Xianshuihe fault (Fig. 1); and lower. but
significant, rates of several mm/a characterize other left-lateral faults. The thrust
faulting docs not seem to have been studied as much as the strike-slip faulting.
but the ...
the Altyn Tagh, the Kunlun and the Xianshuihe fault (Fig. 1); and lower. but
significant, rates of several mm/a characterize other left-lateral faults. The thrust
faulting docs not seem to have been studied as much as the strike-slip faulting.
but the ...
Page 43
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west ... Eastsoutheast striking right -
lateral strike - slip faults are especially clear between northern and southern Tibet
.
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west ... Eastsoutheast striking right -
lateral strike - slip faults are especially clear between northern and southern Tibet
.
Page 49
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west ... Eastsoutheast striking right -
lateral strike - slip faults are especially clear between northern and southern Tibet
.
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west ... Eastsoutheast striking right -
lateral strike - slip faults are especially clear between northern and southern Tibet
.
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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