Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 70
Lithofacies association Internal structure and contact relationship Biogenic
activity Trace fossils ( rare ) Shale with sandstone and limestone Thinly bedded
parallel lamination Limestone with volcanic flows Thinly bedded ( 5-10 cm )
contact ...
Lithofacies association Internal structure and contact relationship Biogenic
activity Trace fossils ( rare ) Shale with sandstone and limestone Thinly bedded
parallel lamination Limestone with volcanic flows Thinly bedded ( 5-10 cm )
contact ...
Page 134
The Kargil molasse of conglomerate and sandstone with occasional shale bands
and coaly layers rests unconformbly over the ganitoids of Ladakh plutonic
complex. The latter forms a NW-SE trending 30 km-wide ganodiorite-diorite
batholith ...
The Kargil molasse of conglomerate and sandstone with occasional shale bands
and coaly layers rests unconformbly over the ganitoids of Ladakh plutonic
complex. The latter forms a NW-SE trending 30 km-wide ganodiorite-diorite
batholith ...
Page 134
Cretaceous to Lower Eocene age is made up of thickly Along the southern
margin of the ITSZ , the bedded sandstone , conglomerate , siltstone and shale (
Pal Lamayuru Formation is separated from TSZ by et al . , 1978 ; Thakur , 1981 ) .
Cretaceous to Lower Eocene age is made up of thickly Along the southern
margin of the ITSZ , the bedded sandstone , conglomerate , siltstone and shale (
Pal Lamayuru Formation is separated from TSZ by et al . , 1978 ; Thakur , 1981 ) .
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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