Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 14
The Zanskar Crystalline Massif ( ZCM ) show that it was upfaulted during late
Proterozoic around 650 Ma ago . This uplift was short lived and again
sedimentation continued upto mid . Cambrian . But then the sea surrounded it on
three sides ...
The Zanskar Crystalline Massif ( ZCM ) show that it was upfaulted during late
Proterozoic around 650 Ma ago . This uplift was short lived and again
sedimentation continued upto mid . Cambrian . But then the sea surrounded it on
three sides ...
Page 21
Foraminiferal Biostratigraphy of the Upper Cretaceous - Lower Tertiary sequence
of the Kharnak - Yarla Area , Zanskar Tethyan Zone , Ladakh Himalaya N.S.
MATHUR & K.P.JUYAL Wadia Institute of Himalayan Geology , Dehra Dun -
248001 ...
Foraminiferal Biostratigraphy of the Upper Cretaceous - Lower Tertiary sequence
of the Kharnak - Yarla Area , Zanskar Tethyan Zone , Ladakh Himalaya N.S.
MATHUR & K.P.JUYAL Wadia Institute of Himalayan Geology , Dehra Dun -
248001 ...
Page 31
1883. The geology of Kashmir and Chamba territories and the British District of
Khangan . Mem . Geol . Surv . India , 22 , 108-112 . Fuchs , G. , 1982. The
geology of western Zanskar . Jahrb . Geol . Bundesanstalt ( Wien ) , 125 , 1-50 .
1986.
1883. The geology of Kashmir and Chamba territories and the British District of
Khangan . Mem . Geol . Surv . India , 22 , 108-112 . Fuchs , G. , 1982. The
geology of western Zanskar . Jahrb . Geol . Bundesanstalt ( Wien ) , 125 , 1-50 .
1986.
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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 |
14 other sections not shown
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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