Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 134
A separate lithostratigaphic unit of the Nindam Formation lies between two
ophiolitic melange belts. The Nindam Formation is of Cretaceous age and may
represent trench sediments (Thakur & Misra, I983). North of the Nindam
Formation, the ...
A separate lithostratigaphic unit of the Nindam Formation lies between two
ophiolitic melange belts. The Nindam Formation is of Cretaceous age and may
represent trench sediments (Thakur & Misra, I983). North of the Nindam
Formation, the ...
Page 134
A separate lithostratigraphic unit of the sides of the thrust . ... It consists of three
units conglomerate and sandstone with occasional shale bands which are
informally designated as unit A , B and C. and coaly layers rests unconformbly
over the ...
A separate lithostratigraphic unit of the sides of the thrust . ... It consists of three
units conglomerate and sandstone with occasional shale bands which are
informally designated as unit A , B and C. and coaly layers rests unconformbly
over the ...
Page 137
Uhramafic lenses . Melange Unit : 4. Shergol Conglomerate : 5. Melange
formation , 6 . Shergol blueschist zone . Higher Himalayan Unit : 7. Karamba and
Lamayuru Unit , 8. Zanskar Unit , ( Modified after Honegger et al . , 1989 ) . v v V
GOMA ...
Uhramafic lenses . Melange Unit : 4. Shergol Conglomerate : 5. Melange
formation , 6 . Shergol blueschist zone . Higher Himalayan Unit : 7. Karamba and
Lamayuru Unit , 8. Zanskar Unit , ( Modified after Honegger et al . , 1989 ) . v v V
GOMA ...
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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