Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 147
The area is classifiable into two units namely i) the Parautochthonous belt in the
south, and, (ii) the Kashmir Synclinorium (Kashmir Nappe) in the north, brought in
juxtaposition along a major tectonic plane referred to as Panjal thrust whose ...
The area is classifiable into two units namely i) the Parautochthonous belt in the
south, and, (ii) the Kashmir Synclinorium (Kashmir Nappe) in the north, brought in
juxtaposition along a major tectonic plane referred to as Panjal thrust whose ...
Page 155
Panjal Volcanic Formation: The Agglomeratic Slate along with Gondwana plant
bearing beds towards its top are ... The fault is sympathetic to Panjal Thrust and
appears to have bifurcated fi'om the latter near Badar west of Saldhar (33° l8' 41"
...
Panjal Volcanic Formation: The Agglomeratic Slate along with Gondwana plant
bearing beds towards its top are ... The fault is sympathetic to Panjal Thrust and
appears to have bifurcated fi'om the latter near Badar west of Saldhar (33° l8' 41"
...
Page 156
Jangpangi et al., 1986 in conformity with the views of Calkins et al., 1975
redesignated the Panjal Thrust as Panjal Fault in view of its steep inclination.
Since the term Panjal Thrust is well entrenched in the geological literature, the
authors ...
Jangpangi et al., 1986 in conformity with the views of Calkins et al., 1975
redesignated the Panjal Thrust as Panjal Fault in view of its steep inclination.
Since the term Panjal Thrust is well entrenched in the geological literature, the
authors ...
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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