Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 107
At margins , the porphyries are deformed whereas in the core they are
undeformed or less deformed . In and around the village Ramgarh , the
porphyries are intensely mylonitised and have developed a foliated structure
resulting into lenticular ...
At margins , the porphyries are deformed whereas in the core they are
undeformed or less deformed . In and around the village Ramgarh , the
porphyries are intensely mylonitised and have developed a foliated structure
resulting into lenticular ...
Page 134
Along the southern margin of the ITSZ, the Lamayuru Formation is separated
from TSZ by SW-dipping Zanskar Thrust. It consists of three units which are
informally designated as unit A, B and C. Along the southern margin, unit 'A'
comprises of ...
Along the southern margin of the ITSZ, the Lamayuru Formation is separated
from TSZ by SW-dipping Zanskar Thrust. It consists of three units which are
informally designated as unit A, B and C. Along the southern margin, unit 'A'
comprises of ...
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