Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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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 71
6 ) whereas in the south , chert and carbonate are present . These carbonates
vary in thickness from 10 to 90 cm and are light grey , cream and black coloured .
The limestone and red shale also show small scale faulting ( Fig . 7 ) .
6 ) whereas in the south , chert and carbonate are present . These carbonates
vary in thickness from 10 to 90 cm and are light grey , cream and black coloured .
The limestone and red shale also show small scale faulting ( Fig . 7 ) .
Page 74
They show sharp basal contact in the thinly bedded sequence , whereas low
relief erosional surfaces are present in thickly to massive limestone . Fossils are
rare and intraclast were also observed at certain levels Cherty limestone is ...
They show sharp basal contact in the thinly bedded sequence , whereas low
relief erosional surfaces are present in thickly to massive limestone . Fossils are
rare and intraclast were also observed at certain levels Cherty limestone is ...
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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