Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 9
Journal of Himalayan Geology , Vol . 5 ( 1 ) , 1994 , pp . 11-19 . Printed in India
Basement Structures and their possible relation to Sedimentation and Tectonics
in the Tethyan Basin of Western Himalaya N.S. VIRDI Wadia Institute of
Himalayan ...
Journal of Himalayan Geology , Vol . 5 ( 1 ) , 1994 , pp . 11-19 . Printed in India
Basement Structures and their possible relation to Sedimentation and Tectonics
in the Tethyan Basin of Western Himalaya N.S. VIRDI Wadia Institute of
Himalayan ...
Page 47
Mesoscopic structures The structures of mesoscopic scale present in the area
have been grouped into planar structures , linear structures , and folds . Planar
fabrics and , at times , it is also observable in Krol and Tal formations . Generally ,
the ...
Mesoscopic structures The structures of mesoscopic scale present in the area
have been grouped into planar structures , linear structures , and folds . Planar
fabrics and , at times , it is also observable in Krol and Tal formations . Generally ,
the ...
Page 53
Era Period Orogeny Main Structural features H DA Deformation Transverse and
oblique faults . ... directions simultaneously , and the maximum finite elongation
direction is almost N - S . Boudinage structures are also observed on microscopic
...
Era Period Orogeny Main Structural features H DA Deformation Transverse and
oblique faults . ... directions simultaneously , and the maximum finite elongation
direction is almost N - S . Boudinage structures are also observed on microscopic
...
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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