Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 65
... Dehra Dun - 248 001 , India Abstract : The Eastern Karakorum was explored
during 1993 by the authors between Sasoma to Depsang La . The Karakorum
fault , marks the southern limit of this traverse , that runs through the Nubra Valley
.
... Dehra Dun - 248 001 , India Abstract : The Eastern Karakorum was explored
during 1993 by the authors between Sasoma to Depsang La . The Karakorum
fault , marks the southern limit of this traverse , that runs through the Nubra Valley
.
Page 67
Sedimentary Belt Southern part of the Karakorum is dominated by a granitoid
batholith nearly 30 km wide , exposed between the Nubra river in the south and
the Upper Shyok river to the north . A metasedimentary envelop occur on either
side ...
Sedimentary Belt Southern part of the Karakorum is dominated by a granitoid
batholith nearly 30 km wide , exposed between the Nubra river in the south and
the Upper Shyok river to the north . A metasedimentary envelop occur on either
side ...
Page 134
Cretaceous to Lower Eocene age is made up of thickly Along the southern
margin of the ITSZ , the bedded sandstone , conglomerate , siltstone and shale (
Pal Lamayuru Formation is separated from TSZ by et al . , 1978 ; Thakur , 1981 ) .
Cretaceous to Lower Eocene age is made up of thickly Along the southern
margin of the ITSZ , the bedded sandstone , conglomerate , siltstone and shale (
Pal Lamayuru Formation is separated from TSZ by et al . , 1978 ; Thakur , 1981 ) .
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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