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 117
Geology of the area ( a ) Upper permafrost zone - lying above the tree line ( 3500
m ) and represented by snow covered peaks ... The Jutogh coinsists of high
grade metamorphics while the Chail represents the low grade metamorphic rocks
.
Geology of the area ( a ) Upper permafrost zone - lying above the tree line ( 3500
m ) and represented by snow covered peaks ... The Jutogh coinsists of high
grade metamorphics while the Chail represents the low grade metamorphic rocks
.
Page 175
Thus , these waveforms largely represent the complexity of the fracturing process
during the earthquake . ... The earthquake source is represented by a
superposition of a number of point dislocation sources distributed over the model
fault ...
Thus , these waveforms largely represent the complexity of the fracturing process
during the earthquake . ... The earthquake source is represented by a
superposition of a number of point dislocation sources distributed over the model
fault ...
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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