Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 41
Page 21
Foraminiferal Biostratigraphy of the Upper Cretaceous - Lower Tertiary sequence
of the Kharnak - Yarla Area , Zanskar Tethyan Zone , Ladakh Himalaya N.S.
MATHUR & K.P.JUYAL Wadia Institute of Himalayan Geology , Dehra Dun -
248001 ...
Foraminiferal Biostratigraphy of the Upper Cretaceous - Lower Tertiary sequence
of the Kharnak - Yarla Area , Zanskar Tethyan Zone , Ladakh Himalaya N.S.
MATHUR & K.P.JUYAL Wadia Institute of Himalayan Geology , Dehra Dun -
248001 ...
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 159
Cambro - Silurian sequence of south - west Kashmir does not support the
magnitude of unconformity proposed by Wadia . criteria for assignment of ages to
these rocks . The recent find of skeletal micro - fossils of Precambrian / Cambrian
...
Cambro - Silurian sequence of south - west Kashmir does not support the
magnitude of unconformity proposed by Wadia . criteria for assignment of ages to
these rocks . The recent find of skeletal micro - fossils of Precambrian / Cambrian
...
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