Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 51
The detrital or primary matrix consists of clay and silt size materials of quartz ,
mica , feldspars and heavy minerals often ... evident , the fact that clay particles
are not mixed up with other mineral grains in the void suggests their diagentic
origin .
The detrital or primary matrix consists of clay and silt size materials of quartz ,
mica , feldspars and heavy minerals often ... evident , the fact that clay particles
are not mixed up with other mineral grains in the void suggests their diagentic
origin .
Page 172
Textural relationship suggests that fibrolite must have formed later after the
formation of other coarse grained minerals . ... In this area , the high grade
mineral assemblages with coarse grained sillimanite might have formed during M
...
Textural relationship suggests that fibrolite must have formed later after the
formation of other coarse grained minerals . ... In this area , the high grade
mineral assemblages with coarse grained sillimanite might have formed during M
...
Page 138
Mineral . Petrol . , 48 , 89-114 . DIETRICH , R. V. 1961. Comments on the two
feldspars geothermometry and K - feldspar obliquity , Cursillos y Conferencias ,
Inst . Lucas Mallada , 8 , 9-13 . FINNEY , J. J. & BAILEY , S. W. 1984. Crystal
structure ...
Mineral . Petrol . , 48 , 89-114 . DIETRICH , R. V. 1961. Comments on the two
feldspars geothermometry and K - feldspar obliquity , Cursillos y Conferencias ,
Inst . Lucas Mallada , 8 , 9-13 . FINNEY , J. J. & BAILEY , S. W. 1984. Crystal
structure ...
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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