Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 169
Both primary and secondary chlorite exists in the chlorite - biotite zone in the
Lower Crystallines , whereas secondary chlorites are observed in the Middle
Crystallines . From the above mineralogical assemblages it is very clear that ...
Both primary and secondary chlorite exists in the chlorite - biotite zone in the
Lower Crystallines , whereas secondary chlorites are observed in the Middle
Crystallines . From the above mineralogical assemblages it is very clear that ...
Page 210
Daviesina tenuis - Lockharria conditi - cerioporids zone ( zone A ) Subarhu
Formation indica , Cythereis rajnathi , Hermanites wadiai , Quadracythere sahnii ,
and Cytherella tawaica . The other taxa included Krithe indica Tewari and
Tandon ...
Daviesina tenuis - Lockharria conditi - cerioporids zone ( zone A ) Subarhu
Formation indica , Cythereis rajnathi , Hermanites wadiai , Quadracythere sahnii ,
and Cytherella tawaica . The other taxa included Krithe indica Tewari and
Tandon ...
Page 11
Initial subduction model is proposed along the Chillien Suture Zone in Central
China . A southward younging of subduction has been noticed . Under this
scheme , if the Shyok Zone is a subduction zone it represents an older
subduction than ...
Initial subduction model is proposed along the Chillien Suture Zone in Central
China . A southward younging of subduction has been noticed . Under this
scheme , if the Shyok Zone is a subduction zone it represents an older
subduction than ...
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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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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