Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 18
D2 folds are associated with well developed S2 axialplane foliation . Crenulation
lineation L2 is well marked and associated with the D2 folds . Crenulation
foliation is parallel to S2 and show shearing . Pucker lineation L2 is well marked
and ...
D2 folds are associated with well developed S2 axialplane foliation . Crenulation
lineation L2 is well marked and associated with the D2 folds . Crenulation
foliation is parallel to S2 and show shearing . Pucker lineation L2 is well marked
and ...
Page 27
Other facies associated with them are scour surface ( Ss ) with a maximum relief
1.5 m consisting of intraformational mud clasts , small pellets of calcareous
mudstone and the calcrete . Lesser amount of planar cross - stratified sandstone
facies ...
Other facies associated with them are scour surface ( Ss ) with a maximum relief
1.5 m consisting of intraformational mud clasts , small pellets of calcareous
mudstone and the calcrete . Lesser amount of planar cross - stratified sandstone
facies ...
Page 61
The first episode of metamorphism ( M ) has reached upto the upper amphibolite
facies and formation of kyanite and sillimanite is associated with this episode .
This episode progressed syn - kinematically with thrusting represented by shear
...
The first episode of metamorphism ( M ) has reached upto the upper amphibolite
facies and formation of kyanite and sillimanite is associated with this episode .
This episode progressed syn - kinematically with thrusting represented by shear
...
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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