Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 58
Page 148
Verma et al . ( 1986 ) reported the occurrence of a continuous band of Fenestella
Shale with plant fossil bearing beds in Ichni - Gulabgarh area in strike
continuation of the Fenestella Shale of Banihal area . Jangpangi et al . ( 1986 ) ,
classified ...
Verma et al . ( 1986 ) reported the occurrence of a continuous band of Fenestella
Shale with plant fossil bearing beds in Ichni - Gulabgarh area in strike
continuation of the Fenestella Shale of Banihal area . Jangpangi et al . ( 1986 ) ,
classified ...
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 ...
Page 195
One to six cm nodules of black chert occur sporadically in the shale ( Acharyya et
al . , 1989 ; Venkatachala et al . , 1990 ; Tiwari & Azmi , 1992 ) . We concur with
Acharyya et al . ( 1989 ) that cherts most likely formed in place during early ...
One to six cm nodules of black chert occur sporadically in the shale ( Acharyya et
al . , 1989 ; Venkatachala et al . , 1990 ; Tiwari & Azmi , 1992 ) . We concur with
Acharyya et al . ( 1989 ) that cherts most likely formed in place during early ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
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
Other editions - View all
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