Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Printed in India Crustal anatexis and Petrogenesis of the Granitoid Rocks , Chor
Region , Himachal Himalaya VINAY M. CHOUBEY , KEWAL K. SHARMA & D.
RAMESHWAR RAO Wadia Institute of Himalayan Geology , Dehra Dun - 248 001
...
Printed in India Crustal anatexis and Petrogenesis of the Granitoid Rocks , Chor
Region , Himachal Himalaya VINAY M. CHOUBEY , KEWAL K. SHARMA & D.
RAMESHWAR RAO Wadia Institute of Himalayan Geology , Dehra Dun - 248 001
...
Page 37
Type of material Moderate to highly Weathered schist , Highly weathered
formation , heavy weathered rocks strike NW ... sinking zone , water seepage with
sandy clay soil 24 ° NE unfavourable foliation plane Soil debris with weathered
rock ...
Type of material Moderate to highly Weathered schist , Highly weathered
formation , heavy weathered rocks strike NW ... sinking zone , water seepage with
sandy clay soil 24 ° NE unfavourable foliation plane Soil debris with weathered
rock ...
Page 42
Under heavy saturation most of the slides are caused by percolation of rain water
through joints and fractures in rocks . ... It is found that most of the landslides are
rock slides and rock - cum - debris slides , however , some landslides show ...
Under heavy saturation most of the slides are caused by percolation of rain water
through joints and fractures in rocks . ... It is found that most of the landslides are
rock slides and rock - cum - debris slides , however , some landslides show ...
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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