Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 18
Textural relations suggest that the kyanite and sillimanite have grown
subsequent to development of S schistosity during progressive regional
metamorphism . Needles of kyanite are also associated with plagioclase .
Presence of sillimanite ...
Textural relations suggest that the kyanite and sillimanite have grown
subsequent to development of S schistosity during progressive regional
metamorphism . Needles of kyanite are also associated with plagioclase .
Presence of sillimanite ...
Page 174
However , during M2 metamorphism , progressive regional metamorphism
continued , and due to rise of temperature - pressure ... M3 metamorphic episode
correlatable with D3 deformation during which regional retrogression took place .
However , during M2 metamorphism , progressive regional metamorphism
continued , and due to rise of temperature - pressure ... M3 metamorphic episode
correlatable with D3 deformation during which regional retrogression took place .
Page 51
Through a regional work the extent of this metamorphism in geographic space
will become known . Likewise , the nature of the metamorphism through the P - T
space would also be determined . At this stage , these questions remain ...
Through a regional work the extent of this metamorphism in geographic space
will become known . Likewise , the nature of the metamorphism through the P - T
space would also be determined . At this stage , these questions remain ...
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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