Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 52
Near Bairagarh , quartzites and phyllites also exhibit the development of mineral
lineation . ... 3 ) this linear fabric formed due to rotational movement and
developed at right angle to the direction of tectonic transport , is very well
developed in ...
Near Bairagarh , quartzites and phyllites also exhibit the development of mineral
lineation . ... 3 ) this linear fabric formed due to rotational movement and
developed at right angle to the direction of tectonic transport , is very well
developed in ...
Page 62
Main Boundary Fault and longitudinal faults were developed during very late
stages of D3 phase where the ... purely under brittle conditions when earlier
developed longitudinal faults were reactivated and the development of
transverse and ...
Main Boundary Fault and longitudinal faults were developed during very late
stages of D3 phase where the ... purely under brittle conditions when earlier
developed longitudinal faults were reactivated and the development of
transverse and ...
Page 81
Since this alternation has caused the development of fractures in the enclosing k
- feldspar grains , the alteration took place after the ... Myrmekitic quartz has
developed along the border of plagioclase having contact with the K - feldspar .
Since this alternation has caused the development of fractures in the enclosing k
- feldspar grains , the alteration took place after the ... Myrmekitic quartz has
developed along the border of plagioclase having contact with the K - feldspar .
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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