Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 121
Palynological analysis of black soil horizone ( Phadtare , 1988 ) reveals that the
lower most black soil horizon contain pollens of annual open grass and primary
wood . This succeeded by alpine to subalpine flora and purely woody to alpine ...
Palynological analysis of black soil horizone ( Phadtare , 1988 ) reveals that the
lower most black soil horizon contain pollens of annual open grass and primary
wood . This succeeded by alpine to subalpine flora and purely woody to alpine ...
Page 133
Earth Sciences , University of Roorkee , Roorkee - 247 667 , India Abstract :
Strain analysis of extracted pebbles of different lithologies from deformed
conglomerate of the Shergol ophiolite melange of the Indus Suture Zone reveals
that there is ...
Earth Sciences , University of Roorkee , Roorkee - 247 667 , India Abstract :
Strain analysis of extracted pebbles of different lithologies from deformed
conglomerate of the Shergol ophiolite melange of the Indus Suture Zone reveals
that there is ...
Page 144
The strain analysis of the conglomerate from the ophiolitic melange of the ITSZ
reveals no distinctive shape of strain ellipsoid . Strain analysis of pebbles of
conglomerate shows that the shape of the pebbles varies from constrictional type
to the ...
The strain analysis of the conglomerate from the ophiolitic melange of the ITSZ
reveals no distinctive shape of strain ellipsoid . Strain analysis of pebbles of
conglomerate shows that the shape of the pebbles varies from constrictional type
to the ...
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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