Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 9
Of the long and complex geological history , the Upper Proterozoic record ,
though well manifest in the Zanskar - Lahaul - Spiti Basin ( ZLSB ) , is , however ,
punctuated by a number of major and minor breaks in sedimentation , attributed
to ...
Of the long and complex geological history , the Upper Proterozoic record ,
though well manifest in the Zanskar - Lahaul - Spiti Basin ( ZLSB ) , is , however ,
punctuated by a number of major and minor breaks in sedimentation , attributed
to ...
Page 36
In addition, one major fault trending NNW-SSE and several minor faults have
also been observed in this 'area. The general trend of bedding foliation is varying
from NW-SE to NE-SW, dipping at 30°-65° m NE to SE direction. In the field, it is ...
In addition, one major fault trending NNW-SSE and several minor faults have
also been observed in this 'area. The general trend of bedding foliation is varying
from NW-SE to NE-SW, dipping at 30°-65° m NE to SE direction. In the field, it is ...
Page 35
The major causes for such a high frequency of landslides in the area are heavy
rainfall and immature topography of the terrain . The paper deals with an analysis
of existing landslides along the major roads of East Sikkim describing the ...
The major causes for such a high frequency of landslides in the area are heavy
rainfall and immature topography of the terrain . The paper deals with an analysis
of existing landslides along the major roads of East Sikkim describing the ...
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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