Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 14
Chenab crystalline The Chenab crystalline are divided into three formations on
the basis of lithostratigraphy and grade of metamorphism . These formations are :
Padar formation , Liond formation and Atholi formation . Padar formation : The ...
Chenab crystalline The Chenab crystalline are divided into three formations on
the basis of lithostratigraphy and grade of metamorphism . These formations are :
Padar formation , Liond formation and Atholi formation . Padar formation : The ...
Page 209
The Subathu Formation of the north west Himalaya is well known for its prolific
molluscan and foraminiferal fauna . However , the ostracode fauna of this
formation has not received much attention from micropalaeontologists . In the
Shimla ...
The Subathu Formation of the north west Himalaya is well known for its prolific
molluscan and foraminiferal fauna . However , the ostracode fauna of this
formation has not received much attention from micropalaeontologists . In the
Shimla ...
Page 213
The Tenga and Dedza formations along with granitic gneiss have developed
chlorite and sericite indicative of lower ... The Bomdila Group has been earlier
called as Tenga Group or Formation but now has been elevated to the status of
group ...
The Tenga and Dedza formations along with granitic gneiss have developed
chlorite and sericite indicative of lower ... The Bomdila Group has been earlier
called as Tenga Group or Formation but now has been elevated to the status of
group ...
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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