Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 127
Later on Bhargava (I980) revised their opinion and extended the window further
east upto Karchham. According to him the quartzite band eiqaosed at Karchham
represents extension of Rampur .Quartzite. However, there are several maps ...
Later on Bhargava (I980) revised their opinion and extended the window further
east upto Karchham. According to him the quartzite band eiqaosed at Karchham
represents extension of Rampur .Quartzite. However, there are several maps ...
Page 131
In addition, the following field and petrogaphic observations are significant in
understanding the true nature of these quartzite units: (1) The Rampur quartzite is
associated with penecontemporaneous basic volcanics (chlorite schist), whereas
...
In addition, the following field and petrogaphic observations are significant in
understanding the true nature of these quartzite units: (1) The Rampur quartzite is
associated with penecontemporaneous basic volcanics (chlorite schist), whereas
...
Page 151
The clasts ranging in size from 1 mm to 30 cms in the diamictite are mainly of vein
quartz, quartzite and slate. Sincha Formation (Jangpangi et al., I986): The
Ramban Formation is overlain by a thin band of orthoquartzite-carbonate rocks ...
The clasts ranging in size from 1 mm to 30 cms in the diamictite are mainly of vein
quartz, quartzite and slate. Sincha Formation (Jangpangi et al., I986): The
Ramban Formation is overlain by a thin band of orthoquartzite-carbonate rocks ...
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Contents
Cnouasv KEWAL K SHARMA D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 21 |
G S MEHROTRA S SARKAR D P KANUNGO A geological appraisal of Landslide Hazards | 35 |
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Common terms and phrases
02:53 IST MAGNITUDE acanthomorphic acritarchs Agglomeratic Slate Amritpur axial plane Bafliaz Formation band basin biotite Budhal calcite chert classified clasts conglomerate defined deformation Dehra Dun deposits diamictite dolomite Doushantuo Formation Dum Gali Quartzite facies fault plane feldspar fi'om field figure fine first flank flows folds foliation fossils Garhwal Geol glacial gneiss granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation lndia lnfrakrol metamorphic Nappe ofthe Panjal thrust Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone schist sector sedimentary sediments sequence shale Sharma shear Shergol significance SiO2 slide slip slope soil stratigraphic structures Surv Suture Zone tectonic Tethyan Thakur thick Thinly bedded Uhl valley unconformably upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Zanskar