Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 147
( 1978 ) reported trilobite trace fossils ( Cruziana and Rusophycus ) from the
Bafliaz Formation ( Wadia's Dogra Slate ) in Thanna Mandi area of Rajauri district
, on the basis of which they assigned Lower Palaeozoic age to the formation .
( 1978 ) reported trilobite trace fossils ( Cruziana and Rusophycus ) from the
Bafliaz Formation ( Wadia's Dogra Slate ) in Thanna Mandi area of Rajauri district
, on the basis of which they assigned Lower Palaeozoic age to the formation .
Page 148
( 1986 ) reported the occurrence of a continuous band of Fenestella Shale with
plant fossil bearing beds in Ichni - Gulabgarh area in strike continuation of the
Fenestella Shale of Banihal area . Jangpangi et al . ( 1986 ) , classified the rocks
in ...
( 1986 ) reported the occurrence of a continuous band of Fenestella Shale with
plant fossil bearing beds in Ichni - Gulabgarh area in strike continuation of the
Fenestella Shale of Banihal area . Jangpangi et al . ( 1986 ) , classified the rocks
in ...
Page 195
Poorly preserved microfossils of broadly Proterozoic aspect have been reported
from the Blaini Formation ( Dhondiyal & Moitra , 1987 ; Joshi et al . , 1988 ) . A
late Proterozoic depositional age has also been inferred on the basis of
Prokaryotic ...
Poorly preserved microfossils of broadly Proterozoic aspect have been reported
from the Blaini Formation ( Dhondiyal & Moitra , 1987 ; Joshi et al . , 1988 ) . A
late Proterozoic depositional age has also been inferred on the basis of
Prokaryotic ...
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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