Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 59
The likely occurrence of a major earthquake associated with 10 m of slip
sometime before 1900 A.D. , after which the historic record for such earthquakes
should be complete , but since 1500 A.D. and probably since 1700 A.D. , allows
for an ...
The likely occurrence of a major earthquake associated with 10 m of slip
sometime before 1900 A.D. , after which the historic record for such earthquakes
should be complete , but since 1500 A.D. and probably since 1700 A.D. , allows
for an ...
Page 70
Whereas segments of the fault and slip associated with each was Molnar and
Deng ( 1984 ) assumed 4 m of oblique left - lateral . Finally , large components of
left - lateral slip reverse faulting , the preponderance of strike - slip on northwest ...
Whereas segments of the fault and slip associated with each was Molnar and
Deng ( 1984 ) assumed 4 m of oblique left - lateral . Finally , large components of
left - lateral slip reverse faulting , the preponderance of strike - slip on northwest ...
Page 113
The first generation of axial planes ( S3 ) associated with F , folds are planar in
small - scale folds ( Fig . 2d and 2h ) but are curved due to subsequent phase of
folding when traced in slightly bigger folds ( Fig . 2b and 2i ) . Sz is evenly ...
The first generation of axial planes ( S3 ) associated with F , folds are planar in
small - scale folds ( Fig . 2d and 2h ) but are curved due to subsequent phase of
folding when traced in slightly bigger folds ( Fig . 2b and 2i ) . Sz is evenly ...
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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