Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 83
The extradolomicrite ( limestone conglomerate ) contains subrounded to rounded
clasts of biomicrite , pelmicrite , bioclasts ... The conglomerate facies contain
coarse sand size clasts of micrite , biomicrite , dismicrite , chert , calcite and rarely
...
The extradolomicrite ( limestone conglomerate ) contains subrounded to rounded
clasts of biomicrite , pelmicrite , bioclasts ... The conglomerate facies contain
coarse sand size clasts of micrite , biomicrite , dismicrite , chert , calcite and rarely
...
Page 85
This lithology contains pockets of fossiliferous and oolitic carbonates ( Table 6 ) .
... These types contain millimeter sized layers of intrasparudite and algal mats
with stromatactis in type A ; micrites , pelsparite and algal mats with stromatactis
in ...
This lithology contains pockets of fossiliferous and oolitic carbonates ( Table 6 ) .
... These types contain millimeter sized layers of intrasparudite and algal mats
with stromatactis in type A ; micrites , pelsparite and algal mats with stromatactis
in ...
Page 149
The phyllitic slates and phyllites occurring in the basal part of the formation
generally contain vein quartz stretched into boudins due to tectonic impress .
Thin laminations exhibiting disharmonic pattern of folding preserved in the
phyllites ...
The phyllitic slates and phyllites occurring in the basal part of the formation
generally contain vein quartz stretched into boudins due to tectonic impress .
Thin laminations exhibiting disharmonic pattern of folding preserved in the
phyllites ...
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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