Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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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 148
( 1986 ) , classified the rocks in the ' Autochthonous Folded belt ' into Gamir ,
Baila , Ramban , Bhimdasa , Sincha , Agglomeratic Slate , Panjal Volcanic ,
Zewan , Poonch Mandi and Rajpur formations and assigned Precambrian age to
the ...
( 1986 ) , classified the rocks in the ' Autochthonous Folded belt ' into Gamir ,
Baila , Ramban , Bhimdasa , Sincha , Agglomeratic Slate , Panjal Volcanic ,
Zewan , Poonch Mandi and Rajpur formations and assigned Precambrian age to
the ...
Page 156
Since the term Panjal Thrust is well entrenched in the geological literature , the
authors have prefered to retain this designation . as The tectonic classification of
Lesser Himalaya into two tectonic units , the ' Autochthonous Folded Belt ' and
the ...
Since the term Panjal Thrust is well entrenched in the geological literature , the
authors have prefered to retain this designation . as The tectonic classification of
Lesser Himalaya into two tectonic units , the ' Autochthonous Folded Belt ' and
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 |
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