Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 58
The eastern third of the Altyn Tagh fault, which follows the north-west boundary of
the Nan Shan, is less clearly delineated by the topography seen on the Landsat
imagery than are the western portions of the fault. Nevertheless, evidence for a ...
The eastern third of the Altyn Tagh fault, which follows the north-west boundary of
the Nan Shan, is less clearly delineated by the topography seen on the Landsat
imagery than are the western portions of the fault. Nevertheless, evidence for a ...
Page 59
Recall that , at 10-12 ka , a relatively wet climate prevailed in the presently very
dry western United States ; perhaps a similar climate , much wetter than now ,
characterized that time in northern Tibet also . The present lack of accurate dating
...
Recall that , at 10-12 ka , a relatively wet climate prevailed in the presently very
dry western United States ; perhaps a similar climate , much wetter than now ,
characterized that time in northern Tibet also . The present lack of accurate dating
...
Page 211
Contributions to Himalayan Geology : Geology of Western Himalaya , Hindustan
Publishing Corporation Delhi , 3 , 52-61 . ... The Mio - Plio - Pleistocene litho -
and biostratigraphy of Surai Khola Siwaliks in West Nepal : First results , C. R.
Acad ...
Contributions to Himalayan Geology : Geology of Western Himalaya , Hindustan
Publishing Corporation Delhi , 3 , 52-61 . ... The Mio - Plio - Pleistocene litho -
and biostratigraphy of Surai Khola Siwaliks in West Nepal : First results , C. R.
Acad ...
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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