Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 102
The average length of the paper including references and text figures should not
exceed more than 20 pages. Thrde complete copies of the manuscript should be
submitted by registered post. Typescripts must be accurate and in their final ...
The average length of the paper including references and text figures should not
exceed more than 20 pages. Thrde complete copies of the manuscript should be
submitted by registered post. Typescripts must be accurate and in their final ...
Page 166
The seismotectonic character of the region is shown in figure la, where it is noted
that the region is laced with thrust faults forming the three main systems
described above. The seismicity, depicted in the figure, comprises of smaller
magnitude ...
The seismotectonic character of the region is shown in figure la, where it is noted
that the region is laced with thrust faults forming the three main systems
described above. The seismicity, depicted in the figure, comprises of smaller
magnitude ...
Page 188
1.0 2.40 136.2 93.3 97.1 134.7 0.5 1.71 136.5 66.0 69.5 95.8 0.3 1.46 135.7 57.0
58.5 81.7 The waveforms, the rupture time contour map, and the total slip
amplitude distribution for the above three inversions are shown in figures 7-9. In
the (a) ...
1.0 2.40 136.2 93.3 97.1 134.7 0.5 1.71 136.5 66.0 69.5 95.8 0.3 1.46 135.7 57.0
58.5 81.7 The waveforms, the rupture time contour map, and the total slip
amplitude distribution for the above three inversions are shown in figures 7-9. In
the (a) ...
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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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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