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
Since most of the pelitic index minerals display two phases of growth history,
probably, the second generation garnet and staurolite are crystallized during M2
metamorphic event. Textural character indicate that these minerals were
crystallized ...
Since most of the pelitic index minerals display two phases of growth history,
probably, the second generation garnet and staurolite are crystallized during M2
metamorphic event. Textural character indicate that these minerals were
crystallized ...
Page 68
The positive correlation of Sr with Ca indicates that their concentration is mainly
controlled by plagioclase. The High Field Strength (HFS) elements like Zr, Y and
Nb are considered to be immobile as they are not usually transported in aqueous
...
The positive correlation of Sr with Ca indicates that their concentration is mainly
controlled by plagioclase. The High Field Strength (HFS) elements like Zr, Y and
Nb are considered to be immobile as they are not usually transported in aqueous
...
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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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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