Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 133
Strain Patterns of the Shergol Ophiolite Melange of the Indus Suture Zone ,
Ladakh R.C. PATEL ' & A.K. JAIN2 ' Wadia Institute of Himalayan Geology ,
Dehra Dun - 248 001 India * 2 Deptt . Earth Sciences , University of Roorkee ,
Roorkee ...
Strain Patterns of the Shergol Ophiolite Melange of the Indus Suture Zone ,
Ladakh R.C. PATEL ' & A.K. JAIN2 ' Wadia Institute of Himalayan Geology ,
Dehra Dun - 248 001 India * 2 Deptt . Earth Sciences , University of Roorkee ,
Roorkee ...
Page 137
The magnitude and symmetry of the strain control the final shape of the pebbles .
Hence , the strain data of the deformed pebbles have been plotted on the polar
graph of Hsu ( 1966 ) . In this graph , the amount of strain ( es ) as the radial ...
The magnitude and symmetry of the strain control the final shape of the pebbles .
Hence , the strain data of the deformed pebbles have been plotted on the polar
graph of Hsu ( 1966 ) . In this graph , the amount of strain ( es ) as the radial ...
Page 144
The strain analysis of the conglomerate from the ophiolitic melange of the ITSZ
reveals no distinctive shape of strain ellipsoid . Strain analysis of pebbles of
conglomerate shows that the shape of the pebbles varies from constrictional type
to the ...
The strain analysis of the conglomerate from the ophiolitic melange of the ITSZ
reveals no distinctive shape of strain ellipsoid . Strain analysis of pebbles of
conglomerate shows that the shape of the pebbles varies from constrictional type
to 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 |
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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