Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 47
Generally , the slaty cleavages are parallel to the bedding plane . In the phyllites
of Garhwal Nappe S , is uniformaly developed and characterized by preferred
orientation of the flaky minerals like chlorite and white micas , alternating with ...
Generally , the slaty cleavages are parallel to the bedding plane . In the phyllites
of Garhwal Nappe S , is uniformaly developed and characterized by preferred
orientation of the flaky minerals like chlorite and white micas , alternating with ...
Page 61
In the present area , a well demarcated thrust plane can be easily recognized by
the appearance of metamorphic rocks i.e. , phyllites and quartzites of Garhwal
Nappe , overlying unmetamophosed rocks i.e. shales and limestones belonging
to ...
In the present area , a well demarcated thrust plane can be easily recognized by
the appearance of metamorphic rocks i.e. , phyllites and quartzites of Garhwal
Nappe , overlying unmetamophosed rocks i.e. shales and limestones belonging
to ...
Page 188
This will be of .considerable utility in earthquake hazard parameterization . over
the fault plane in the form of variable density plots . The ( c ) parts of the figures
show the slip vector distribution over the fault plane . For the choice of rise time of
1 ...
This will be of .considerable utility in earthquake hazard parameterization . over
the fault plane in the form of variable density plots . The ( c ) parts of the figures
show the slip vector distribution over the fault plane . For the choice of rise time of
1 ...
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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