Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 147
Geology of Thanna Mandi - Ramsu sector of Lesser Himalaya , J & K S.N.
VERMA & K.K. SHARMA Regional Geology Division Geological Survey of India ,
Jammu - 180 004 , India Abstract : Geology of Thanna Mandi - Ramsu sector of
the ...
Geology of Thanna Mandi - Ramsu sector of Lesser Himalaya , J & K S.N.
VERMA & K.K. SHARMA Regional Geology Division Geological Survey of India ,
Jammu - 180 004 , India Abstract : Geology of Thanna Mandi - Ramsu sector of
the ...
Page 158
In the eastern sector , Vohra ( 1958-59 , 1964 , 1966 ) classified the rocks
constituting the upper part of Wadia's Salkhala series and the physically
overlying " Cambro - Silurian " or older series ( Wadia & Das Hazra in Vohra ,
1958-59 , 1964 ) ...
In the eastern sector , Vohra ( 1958-59 , 1964 , 1966 ) classified the rocks
constituting the upper part of Wadia's Salkhala series and the physically
overlying " Cambro - Silurian " or older series ( Wadia & Das Hazra in Vohra ,
1958-59 , 1964 ) ...
Page 159
He ( 1934a , 1936 ) regionalised this unconformity by observing a hiatus between
Salkhala series and the succeeding Fenestella Quartzite / Agglomeratic Slate in
Kandi - Budhal - Gulabgarh sector between Salkhal series / Cambrian and the ...
He ( 1934a , 1936 ) regionalised this unconformity by observing a hiatus between
Salkhala series and the succeeding Fenestella Quartzite / Agglomeratic Slate in
Kandi - Budhal - Gulabgarh sector between Salkhal series / Cambrian and the ...
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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