Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 195
Redeposited sand - sized clasts of microbial mats and acanthomorphic acritarchs
support a shallow subtidal environment of deposition . Petrographically and
paleontologically , the fossiliferous Infrakrol rocks closely resemble cherts of
similar ...
Redeposited sand - sized clasts of microbial mats and acanthomorphic acritarchs
support a shallow subtidal environment of deposition . Petrographically and
paleontologically , the fossiliferous Infrakrol rocks closely resemble cherts of
similar ...
Page 200
Soc . India , 28 , 106-111 . DHONDIYAL , J.N. & MOITRA , A. K. , 1987.
Precambrian acritarchs from Blaini Formation , Garhwal Syncline , Uttar Pradesh .
Indian Minerals , 41 , 1 , 69-74 . LAKHANPAL , R.N. , SAH , S.C.D. & DUBEY ,
S.N. , 1958 ...
Soc . India , 28 , 106-111 . DHONDIYAL , J.N. & MOITRA , A. K. , 1987.
Precambrian acritarchs from Blaini Formation , Garhwal Syncline , Uttar Pradesh .
Indian Minerals , 41 , 1 , 69-74 . LAKHANPAL , R.N. , SAH , S.C.D. & DUBEY ,
S.N. , 1958 ...
Page
Large Acanthomorphic Acritarchs from the Infrakrol Formation of the Lesser
Himalaya and their Stratigraphic Significance 193 Published for the Wadia
Institute of Himalayan Geology , 33 - General Mahadeo Singh Road , Dehra Dun
- 248 001 ...
Large Acanthomorphic Acritarchs from the Infrakrol Formation of the Lesser
Himalaya and their Stratigraphic Significance 193 Published for the Wadia
Institute of Himalayan Geology , 33 - General Mahadeo Singh Road , Dehra Dun
- 248 001 ...
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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