Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 74
The colour of limestone ranges from light green , cream , dark grey to black . It is
also brittle and gives foetid smell on breaking . They show sharp basal contact in
the thinly bedded sequence , whereas low relief erosional surfaces are present ...
The colour of limestone ranges from light green , cream , dark grey to black . It is
also brittle and gives foetid smell on breaking . They show sharp basal contact in
the thinly bedded sequence , whereas low relief erosional surfaces are present ...
Page 153
Earthy brown crystalline limestone with vein quartz and Chunks of schistose
quartzite Greyish white to grey coloured massive to phyllitic and schistose
quartzite Unconformity Bafliaz Formation In Deol ( 33 ° 24 ' 50 " : 74 ° 54 ' 00 ...
Earthy brown crystalline limestone with vein quartz and Chunks of schistose
quartzite Greyish white to grey coloured massive to phyllitic and schistose
quartzite Unconformity Bafliaz Formation In Deol ( 33 ° 24 ' 50 " : 74 ° 54 ' 00 ...
Page 155
bedded , dark grey limestone and 92 meters thick earthy micaceous sandstone .
The rocks are exposed at the Gulabgarh pass on the Pir Panjal range .
Khunamuh Formation ( Nakazawa et al . , 1975 ; Nakazawa & Kapoor , 1981 ) :
The ...
bedded , dark grey limestone and 92 meters thick earthy micaceous sandstone .
The rocks are exposed at the Gulabgarh pass on the Pir Panjal range .
Khunamuh Formation ( Nakazawa et al . , 1975 ; Nakazawa & Kapoor , 1981 ) :
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