Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 147
The tectonic plane , hitherto , considered as the trace of Panjal thrust separating
Carboniferous - Eocene sequence from the so called Dogra Slate in the south -
eastern part of the area ( Chenab valley ) is now named as Saldhar Fault . In view
...
The tectonic plane , hitherto , considered as the trace of Panjal thrust separating
Carboniferous - Eocene sequence from the so called Dogra Slate in the south -
eastern part of the area ( Chenab valley ) is now named as Saldhar Fault . In view
...
Page 155
The rocks are exposed at the Gulabgarh pass on the Pir Panjal range . Structure
The main structural elements in the area are as under : Thrust / Fault have been
reported from the rocks of Sigari Member , which impart Sakmarian ( Lower ...
The rocks are exposed at the Gulabgarh pass on the Pir Panjal range . Structure
The main structural elements in the area are as under : Thrust / Fault have been
reported from the rocks of Sigari Member , which impart Sakmarian ( Lower ...
Page 156
Jangpangi et al . , 1986 in conformity with the views of Calkins et al . , 1975
redesignated the Panjal Thrust as Panjal Fault in view of its steep inclination .
Since the term Panjal Thrust is well entrenched in the geological literature , the
authors ...
Jangpangi et al . , 1986 in conformity with the views of Calkins et al . , 1975
redesignated the Panjal Thrust as Panjal Fault in view of its steep inclination .
Since the term Panjal Thrust is well entrenched in the geological literature , the
authors ...
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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