Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 14
But then the sea surrounded it on three sides i.e. Kashmir , Zanskar and Lahaul -
Spiti . The southern side was uplifted and connected to the Main Indian landmass
. The palaeoslopes were directed away from the central high . Keeping in mind ...
But then the sea surrounded it on three sides i.e. Kashmir , Zanskar and Lahaul -
Spiti . The southern side was uplifted and connected to the Main Indian landmass
. The palaeoslopes were directed away from the central high . Keeping in mind ...
Page 147
The area is classifiable into two units namely i ) the Parautochthonous belt in the
south , and , ( ii ) the Kashmir Synclinorium ( Kashmir Nappe ) in the north ,
brought in juxtaposition along a major tectonic plane referred to as Panjal thrust ...
The area is classifiable into two units namely i ) the Parautochthonous belt in the
south , and , ( ii ) the Kashmir Synclinorium ( Kashmir Nappe ) in the north ,
brought in juxtaposition along a major tectonic plane referred to as Panjal thrust ...
Page 160
Sedimentology of the slate belt of Ramban - Banihal area , Kashmir Himalaya .
Him . Geol . , 3 , 116-134 . PAREEK , H.S. , 1976. On studies of the Agglomeratic
Slate and Panjal Trap in the Jhelum , Liddar and Sind valleys , Kashmir . Rec .
Sedimentology of the slate belt of Ramban - Banihal area , Kashmir Himalaya .
Him . Geol . , 3 , 116-134 . PAREEK , H.S. , 1976. On studies of the Agglomeratic
Slate and Panjal Trap in the Jhelum , Liddar and Sind valleys , Kashmir . Rec .
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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