Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 97
This dolomitic formation along Surnayagad section is much reduced in thickness
. Very frequently thick to thin black carbonaceous slates , green - grey slates and
calcareous sandstones are interbedded within the massive dolomite around ...
This dolomitic formation along Surnayagad section is much reduced in thickness
. Very frequently thick to thin black carbonaceous slates , green - grey slates and
calcareous sandstones are interbedded within the massive dolomite around ...
Page 98
It comprises a thick sequence of quartzites and schists . Compared to the Kali
section , the thickness in the eastern continuation of this group along Chamalya
river is reduced to nearly half . It is preserved in a synform whose axis passess
from ...
It comprises a thick sequence of quartzites and schists . Compared to the Kali
section , the thickness in the eastern continuation of this group along Chamalya
river is reduced to nearly half . It is preserved in a synform whose axis passess
from ...
Page 103
In the Indian subcontinent , evaporites constitute thick horizons in the Salt Range
, Lesser Himalaya in J & K , H.P. and in the Trans - Aravalli Vindhyan basin in
Jaisalmer - Bikaner region . However on the eastern side of the Aravalli massif ...
In the Indian subcontinent , evaporites constitute thick horizons in the Salt Range
, Lesser Himalaya in J & K , H.P. and in the Trans - Aravalli Vindhyan basin in
Jaisalmer - Bikaner region . However on the eastern side of the Aravalli massif ...
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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
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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