Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
From inside the book
Results 1-3 of 85
Page 147
Interpretive cross section across the boundary between the Indo - Gangetic
Plains and the Lesser Himalaya showing the successive detachment of
sedimentary sequences and the ramping of them onto the material farther south .
In the legend ...
Interpretive cross section across the boundary between the Indo - Gangetic
Plains and the Lesser Himalaya showing the successive detachment of
sedimentary sequences and the ramping of them onto the material farther south .
In the legend ...
Page 213
Material : More than eighty specimens . Figured specimen , Cat . No. WIMF / A
432 . Occurrence : Rare to abundant in zones C - F in several blocks of the
Subathu Formation . Paracypris sp . 1 Pl . I , fig . 7 Dimensions ( mm ) : L 0.70 , H
0.30 , W ...
Material : More than eighty specimens . Figured specimen , Cat . No. WIMF / A
432 . Occurrence : Rare to abundant in zones C - F in several blocks of the
Subathu Formation . Paracypris sp . 1 Pl . I , fig . 7 Dimensions ( mm ) : L 0.70 , H
0.30 , W ...
Page 263
The foregoing views of the authors regarding the nature of lithological
associations of the material constituting the Ophiolitic Melange Zone clearly
indicate the dual nature of the Ophiolitic Melange Zone . On the one hand , it
consists of ...
The foregoing views of the authors regarding the nature of lithological
associations of the material constituting the Ophiolitic Melange Zone clearly
indicate the dual nature of the Ophiolitic Melange Zone . On the one hand , it
consists of ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
The Shyok valley Northern Ladakh India An entraped and compressed marginal | 1 |
Chemical mineralogy of the Panjal Traps around Bandipura Kashmir | 17 |
Structural characteristics of the rocks of BanihalRamban area | 23 |
28 other sections not shown
Other editions - View all
Common terms and phrases
activity associated authors basin beds belt biotite block Central correlation Crystallines deformation deposits developed District dolerite earthquakes eastern et al event exposed extends facies fault feldspars field folds followed Formation formed Garhwal Geol Geology gneisses grade grains granite granitoids Group higher Himalaya Himalayan Geology hornblende India indicate Indus Institute Jour Krol Ladakh Late later Lesser Himalaya limestone lower Main major margin material metamorphism Middle minerals nature Nayar northern observed occur oceanic ophiolitic origin phase phyllite plagioclase plane plate Pradesh present quartz quartzite range References region represented result river rocks Salt samples sandstone schist sedimentary sediments sequence Series shale Sharma Shyok Siwalik slip slope southern Spiti structural Subathu subduction suggests surface Suture Table tectonic thick Thrust trend units Upper valley values variation volcanics Wadia western zone