Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 32
Multistoriedness of the sand bodies would indicate repeated stream encounter at
the depositional site . Lateral accretion surfaces are absent . Common
occurrence of reactivation surface ( Fig . 4c ) and large amount of soil carbonate
indicate ...
Multistoriedness of the sand bodies would indicate repeated stream encounter at
the depositional site . Lateral accretion surfaces are absent . Common
occurrence of reactivation surface ( Fig . 4c ) and large amount of soil carbonate
indicate ...
Page 173
Also the idioblastic garnets appear to be growing over S , foliation which is
abuting against the garnet crystals , indicating that these garnets have
crystallized during D2 deformation . Possibly the major thrusting event initiated
between post F ...
Also the idioblastic garnets appear to be growing over S , foliation which is
abuting against the garnet crystals , indicating that these garnets have
crystallized during D2 deformation . Possibly the major thrusting event initiated
between post F ...
Page 68
The variation in grain size and absence of cross cutting relationship and contact
metamorphic aureoles indicate non ... Such variation indicates the involvement of
alkali metasomatism in the transformation of the country rock to migmatites .
The variation in grain size and absence of cross cutting relationship and contact
metamorphic aureoles indicate non ... Such variation indicates the involvement of
alkali metasomatism in the transformation of the country rock to migmatites .
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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 |
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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