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
Textural character indicate that these minerals were crystallized in relation to the
S2 foliation during D2 deformation. In most of ... The cross cutting relationship of
biotite and muscovite with reference to S1 schistosity indicate that these minerals
...
Textural character indicate that these minerals were crystallized in relation to the
S2 foliation during D2 deformation. In most of ... The cross cutting relationship of
biotite and muscovite with reference to S1 schistosity indicate that these minerals
...
Page 68
The positive correlation of Sr with Ca indicates that their concentration is mainly
controlled by plagioclase. ... The variation in grain size and absence of cross
cutting relationship and contact metamorphic aureoles indicate non-magmatic
origin ...
The positive correlation of Sr with Ca indicates that their concentration is mainly
controlled by plagioclase. ... The variation in grain size and absence of cross
cutting relationship and contact metamorphic aureoles indicate non-magmatic
origin ...
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Contents
The Shyok valley Northern Ladakh India An entraped and compressed marginal | 31 |
Megacrysts in the granitoid rocks | 39 |
Shaleslate metamorphism in Yashwant NagarDudhem | 47 |
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Common terms and phrases
amphibolite Amritpur Amritpur Granite basin beds biotite block chlorite clasts conglomerate correlation Cretaceous Crystallines deformation deposits developed dolerite dolomite earthquakes eastern Eocene evaporites facies fault feldspars folds fossils Garhwal Garhwal Himalaya garnet Geol glacial glacier gneisses Gondwana grained granite granitoids Group Himalaya Himalayan Geology hornblende hornblende schists India Indian plate indicate Institute of Himalayan Jour Journal of Himalayan K-feldspar Krol Belt Kumar Kumaun Ladakh Lesser Himalaya limestone lineament lithology lower magmatic margin metamorphism Middle Siwalik migmatites minerals Molnar moraines muscovite Nayar observed occur ophiolitic ophiolitic melange Pakistan phase phyllite plagioclase plane Precambrian quartz quartzite Rawat region river rocks Salt Range samples sandstone schist sedimentary sediments sequence shale Sharma shear zones shows Shyok Singh Siwalik slope Spiti stratigraphic structure Subathu Subathu Formation subduction Surv Suture Zone syncline tectonic Tethyan thick thrust trend Upper Siwalik Valdiya valley volcanics Wadia Institute western