Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 2
The length of the fracture is approx 15 m and it is marked by discontinuity of beds
. The apparent displacement of beds is insignificant and the fracture appears to
be a joint surface . The fault is sinusoidal in the cross - section and the bedding is
...
The length of the fracture is approx 15 m and it is marked by discontinuity of beds
. The apparent displacement of beds is insignificant and the fracture appears to
be a joint surface . The fault is sinusoidal in the cross - section and the bedding is
...
Page 33
Remarks : The original record of this cosmopolitan species comes from the
Eocene beds of France . Keij ( 1957 ) recorded this species from the Eocene
beds of Belgium and Netherlands . In India this species has been recorded from
various ...
Remarks : The original record of this cosmopolitan species comes from the
Eocene beds of France . Keij ( 1957 ) recorded this species from the Eocene
beds of Belgium and Netherlands . In India this species has been recorded from
various ...
Page 34
Remarks : Cytherella lakhpatensis recorded herein closely resembles in all
external characters with those recorded by Khosla and Pant ( 1988 ) from the
early Lutetian beds of Kachchh . Type level and locality : Green nodular shale (
zone ...
Remarks : Cytherella lakhpatensis recorded herein closely resembles in all
external characters with those recorded by Khosla and Pant ( 1988 ) from the
early Lutetian beds of Kachchh . Type level and locality : Green nodular shale (
zone ...
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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