Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 43
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west extension and north - south
shortening ( due to strike - slip , not thrust faulting ) . Eastsoutheast striking right -
lateral ...
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west extension and north - south
shortening ( due to strike - slip , not thrust faulting ) . Eastsoutheast striking right -
lateral ...
Page 44
Thus , while normal faulting and roughly east - west crustal extension occurs in
the high plateau , slip on roughly east - west trending left - lateral strike - slip
faults causes pervasive shear of the northern and eastern margins of Tibet , and ...
Thus , while normal faulting and roughly east - west crustal extension occurs in
the high plateau , slip on roughly east - west trending left - lateral strike - slip
faults causes pervasive shear of the northern and eastern margins of Tibet , and ...
Page 49
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west extension and north - south
shortening ( due to strike - slip , not thrust faulting ) . Eastsoutheast striking right -
lateral ...
Roughly equal amounts of normal and strike - slip faulting occur in the northern
part of the high plateau leading to east - west extension and north - south
shortening ( due to strike - slip , not thrust faulting ) . Eastsoutheast striking right -
lateral ...
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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