Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 74
This facies is generally thinly bedded and bed thickness increases towards top .
The colour of limestone ranges ... Shale in lower part is 150 m thick and is
associated with fine grained , thinly bedded sandstone . Shale is generally dark
grey to ...
This facies is generally thinly bedded and bed thickness increases towards top .
The colour of limestone ranges ... Shale in lower part is 150 m thick and is
associated with fine grained , thinly bedded sandstone . Shale is generally dark
grey to ...
Page 121
6 ) . thick soil horizon has distinct black and brown soil layers buried under 40-60
cm thick recent soil . The thickness of black soil horizon varies from 75 cm near
Kurdhara to 10-20 cm in the entire mid hill slope . At few places these black soil ...
6 ) . thick soil horizon has distinct black and brown soil layers buried under 40-60
cm thick recent soil . The thickness of black soil horizon varies from 75 cm near
Kurdhara to 10-20 cm in the entire mid hill slope . At few places these black soil ...
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