Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 82
The textural details with allochems and faunal distribution was studied for
establishing the microfacies . The classification of Folk ( 1962 ) was followed
throughout the study for microfacies classification . The microfacies were
classified on the ...
The textural details with allochems and faunal distribution was studied for
establishing the microfacies . The classification of Folk ( 1962 ) was followed
throughout the study for microfacies classification . The microfacies were
classified on the ...
Page 83
occurs The volcanic rock includes in general acid volcanics followed by
intermediate volcanic rocks . They consist of feldspar ( plagioclase and
orthoclase ) quartz and basic minerals . Calcite is also present in few samples .
Feldspar occurs ...
occurs The volcanic rock includes in general acid volcanics followed by
intermediate volcanic rocks . They consist of feldspar ( plagioclase and
orthoclase ) quartz and basic minerals . Calcite is also present in few samples .
Feldspar occurs ...
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 ...
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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