Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 45
The area has undergone four phases of deformation . The D , deformation was
responsible for the development of first generation of folding ( F ) , axial planes (
S3 ) and linear fabrics . The D , deformation was responsible for the development
...
The area has undergone four phases of deformation . The D , deformation was
responsible for the development of first generation of folding ( F ) , axial planes (
S3 ) and linear fabrics . The D , deformation was responsible for the development
...
Page 61
During the later tectonic phase the thrust plane was also folded into a broad
synformal structure . ... severe orogenic phases during the Late Precambrian te
Paleocene time is indicated by the rocks of the present area . However , ample ...
During the later tectonic phase the thrust plane was also folded into a broad
synformal structure . ... severe orogenic phases during the Late Precambrian te
Paleocene time is indicated by the rocks of the present area . However , ample ...
Page 62
Second Phase of Deformation ( D2 ) along bedding planes during the formation
of the Garhwal synform . Main Boundary Fault and longitudinal faults were
developed during very late stages of D3 phase where the deformation was under
brittle ...
Second Phase of Deformation ( D2 ) along bedding planes during the formation
of the Garhwal synform . Main Boundary Fault and longitudinal faults were
developed during very late stages of D3 phase where the deformation was under
brittle ...
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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