Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 69
(For Legend see Fig.2) The limestone dominant interval is present in the central
part and is thinly bedded (Fig. 4). At other levels this facies is associated with
sandstone and volcanic flows (Fig. 3). Limestone is grey to green coloured and
has ...
(For Legend see Fig.2) The limestone dominant interval is present in the central
part and is thinly bedded (Fig. 4). At other levels this facies is associated with
sandstone and volcanic flows (Fig. 3). Limestone is grey to green coloured and
has ...
Page 75
Lithofades Internal structure Biogenic Thickness association and contact activity (
in metres) relationship Limestone Thickly bedded (massive in - 50 nature), base
uneven _ Red and green shale Highly cleaved and crumpled - l5 Limestone with
...
Lithofades Internal structure Biogenic Thickness association and contact activity (
in metres) relationship Limestone Thickly bedded (massive in - 50 nature), base
uneven _ Red and green shale Highly cleaved and crumpled - l5 Limestone with
...
Page 78
Field Characteristics of Burtsa Formation Lighofacies Internal structure Biogenic
Thickness association and contact activity (in metres) relationship Limestone and
sandstone Thickly bedded - 75 sharp contact Gypsum with lenses of Thinlyto ...
Field Characteristics of Burtsa Formation Lighofacies Internal structure Biogenic
Thickness association and contact activity (in metres) relationship Limestone and
sandstone Thickly bedded - 75 sharp contact Gypsum with lenses of Thinlyto ...
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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