Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 91
Triassic ( Morgo Formation ) is represented by limestone conglomerate at the
base followed by carbonates and black shale . During lower to Middle Triassic
the deeper water facies assemblage is indicated by geometry , facies and
microfacies ...
Triassic ( Morgo Formation ) is represented by limestone conglomerate at the
base followed by carbonates and black shale . During lower to Middle Triassic
the deeper water facies assemblage is indicated by geometry , facies and
microfacies ...
Page 131
... current bedding extensively present in the Rampur Quartzite are completely
missing in the Karchham Quartzite . The Karchham Quartzite and the overlying
schist and gneiss intercalated with quartzite layers represent cyclic sedimentation
.
... current bedding extensively present in the Rampur Quartzite are completely
missing in the Karchham Quartzite . The Karchham Quartzite and the overlying
schist and gneiss intercalated with quartzite layers represent cyclic sedimentation
.
Page 175
Thus , these waveforms largely represent the complexity of the fracturing process
during the earthquake . The ground velocity waveforms derived by integration of
the accelerograms at the seven sites under consideration ( Figs . 5 ( 1 ) -5 ( 7 ) ...
Thus , these waveforms largely represent the complexity of the fracturing process
during the earthquake . The ground velocity waveforms derived by integration of
the accelerograms at the seven sites under consideration ( Figs . 5 ( 1 ) -5 ( 7 ) ...
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Contents
Petrogenesis of the Granitoid Rocks Chor Region Himachal Himalaya | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
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Common terms and phrases
Agglomeratic Slate analysis associated band base basin bedded belt chert components composition comprising conglomerate contain covered deformation Dehra deposits developed direction distribution district earthquake et al exposed facies fault fault plane feldspar field folds foliation followed Formation fossils Garhwal Geol gneiss grained granites granitoids grey Group higher Himalaya Himalayan Geology India indicates inversion Jour Kashmir Ladakh Lamayuru Late Lesser limestone lineation locality locations lower major Member metamorphic minerals observed occur Panjal pebbles phase phyllites plagioclase plane Pleistocene porphyries present quartz quartzite range region reported represented river road rocks samples sandstone schist sector sedimentary sediments sequence shale Sharma shown Slate slide slip slope soil strain stratigraphy strike structures suggest Surv Table tectonic thick thrust trace unit upper valley VALUES Volcanics Wadia weathered Zanskar zone