Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 21
Based on biostratigraphy of the Goma - Lingshet succession , its geological
history has been deduced from Late Cretaceous to early Tertiary . The above
succession has been compared with equivalent successions in the Spiti region in
the ...
Based on biostratigraphy of the Goma - Lingshet succession , its geological
history has been deduced from Late Cretaceous to early Tertiary . The above
succession has been compared with equivalent successions in the Spiti region in
the ...
Page 29
This zone corresponds to Morozovella edgari to M. subbotinae Zones ( both Early
Ypresian ) . Discussion is represented by the by the shallow shallow marine
Lingshet ( Thanetian - Early Ypresian ) and Kong ( Late Ypresian ) Formations .
This zone corresponds to Morozovella edgari to M. subbotinae Zones ( both Early
Ypresian ) . Discussion is represented by the by the shallow shallow marine
Lingshet ( Thanetian - Early Ypresian ) and Kong ( Late Ypresian ) Formations .
Page 201
The significance and occurrence of late Paleozoic Plant remains in the Infrakrol
sequence of Naini Tal , U.P. Bull . Indian Geol . Assoc . , 12 ( 2 ) , 263-266 . & Li ,
Z. , 1978. Precambrian microfloras of southwest - China with reference to their ...
The significance and occurrence of late Paleozoic Plant remains in the Infrakrol
sequence of Naini Tal , U.P. Bull . Indian Geol . Assoc . , 12 ( 2 ) , 263-266 . & Li ,
Z. , 1978. Precambrian microfloras of southwest - China with reference to their ...
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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