Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 28
Page 199
Chronostratigraphic markers in the end - Precambrian carbon - isotope record of
the Lesser Himalaya . Nature , 327 , 699-702 . Description : Unbranched
filaments 30-76um in cross - sectional diameter and more than 300 um long .
Filaments ...
Chronostratigraphic markers in the end - Precambrian carbon - isotope record of
the Lesser Himalaya . Nature , 327 , 699-702 . Description : Unbranched
filaments 30-76um in cross - sectional diameter and more than 300 um long .
Filaments ...
Page 200
Geol . Soc . India , 39 , 229-234 . BRASIER , M.D. & SINGH , P. , 1987.
Microfossils and PrecambrianCambrian boundry stratigraphy at Maldeota ,
Lesser Himalaya . Geol . Mag , 124 , 323-345 . KUMAR , G. , BHATT , D.K. &
RAINA , B.K. , 1987.
Geol . Soc . India , 39 , 229-234 . BRASIER , M.D. & SINGH , P. , 1987.
Microfossils and PrecambrianCambrian boundry stratigraphy at Maldeota ,
Lesser Himalaya . Geol . Mag , 124 , 323-345 . KUMAR , G. , BHATT , D.K. &
RAINA , B.K. , 1987.
Page 201
Stratigraphy and structural evolution of the Kumaun Lesser Himalaya . Sediment .
Geol . , 81-265 . VENKATACHALA , B.S. , SHUKLA , M. , BANSAL , R. &
ACHARYYA , S.K. , 1990. Upper Proterozoic microfossils from the Infrakrol
sediments ...
Stratigraphy and structural evolution of the Kumaun Lesser Himalaya . Sediment .
Geol . , 81-265 . VENKATACHALA , B.S. , SHUKLA , M. , BANSAL , R. &
ACHARYYA , S.K. , 1990. Upper Proterozoic microfossils from the Infrakrol
sediments ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
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 |
14 other sections not shown
Other editions - View all
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