Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 70
Lithofacies Intemal structure Biogenic Thickness association and contact activity (
in metres) relationship Shale with sandstone Thinly bedded Trace fossils (rare)
400 and limestone parallel lamination Limestone with volcanic flows Thinly ...
Lithofacies Intemal structure Biogenic Thickness association and contact activity (
in metres) relationship Shale with sandstone Thinly bedded Trace fossils (rare)
400 and limestone parallel lamination Limestone with volcanic flows Thinly ...
Page 71
The limestone and red shale also show small scale faulting (Fig. 7). They contain
at places, intraclasts, clasts (Fig. 8) and rarely fossils. Flaggy and laminated
carbonates are also present. Lensoidal carbonate bodies with erosional basal ...
The limestone and red shale also show small scale faulting (Fig. 7). They contain
at places, intraclasts, clasts (Fig. 8) and rarely fossils. Flaggy and laminated
carbonates are also present. Lensoidal carbonate bodies with erosional basal ...
Page 74
Shale in lower part is 150 m thick and is associated with fine grained, thinly
bedded sandstone. Shale is generally dark grey to black coloured, fissile and
highly cleaved. lt is highly folded and crumpled. Laminated shale is present at
various ...
Shale in lower part is 150 m thick and is associated with fine grained, thinly
bedded sandstone. Shale is generally dark grey to black coloured, fissile and
highly cleaved. lt is highly folded and crumpled. Laminated shale is present at
various ...
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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