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Page 400
The mylonitic gneisses generally occur towards the sole of the thrust sheet in ,
more or less , continuous bands . The most characteristic feature is its
continuation on both limbs of the Nirath - Pandoh synform which is
complimentary to the ...
The mylonitic gneisses generally occur towards the sole of the thrust sheet in ,
more or less , continuous bands . The most characteristic feature is its
continuation on both limbs of the Nirath - Pandoh synform which is
complimentary to the ...
Page 401
... bed quartzite , Phy : Mylonitic gneiss llites and quart Mica schist , ( d ) Graphitic
( 10-12 m ) llites , Mylonitic Phyllites and zite , Mylonitic Mylonitic phyllite ( b )
Slightly puckgnesis schists gneisses gneisses ered grey phyllites Chlorite -
sericite ...
... bed quartzite , Phy : Mylonitic gneiss llites and quart Mica schist , ( d ) Graphitic
( 10-12 m ) llites , Mylonitic Phyllites and zite , Mylonitic Mylonitic phyllite ( b )
Slightly puckgnesis schists gneisses gneisses ered grey phyllites Chlorite -
sericite ...
Page 458
Mylonitic granite occurs at the basal part of the Phaplu augen gneiss only in the
northem part. It is coarse grained and have no penetrative foliation, instead the
rock contains peculiar rod-like lineation. Thus, the granite shows its massive ...
Mylonitic granite occurs at the basal part of the Phaplu augen gneiss only in the
northem part. It is coarse grained and have no penetrative foliation, instead the
rock contains peculiar rod-like lineation. Thus, the granite shows its massive ...
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Contents
The Central Himalayan Gneisses in Northern Pakistan | 1 |
LowPressure Metamorphism in a Regionally Metamorphic | 39 |
The Buniyar Granite of the Kashmir Himalaya | 61 |
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Common terms and phrases
Almora angle appears assemblages associated augen axes axial axis bands base bedding belt biotite boundary Chail chlorite cleavage composition consists contain continuous crenulation crystalline deformation developed diagram direction District eastern exposed fabric facies faults folds foliation Formation formed fractures Garhwal garnet Geol Geology girdle gneiss grade grains granite Group higher Himalaya inclusions increase India indicate isograd Jour Jutogh Krol Kumaun kyanite Lesser Himalaya limestone lineation lower Main Central major metamorphism mica migmatites mineral movement muscovite mylonitic nappe Nepal observed occur orientation parallel pelitic phase phyllites plagioclase plane porphyroblasts present pressure quartz quartzite range reaction region relief represented result rocks Saklani schist schistosity sequence sericite sets shear sheet sillimanite similar Siwalik slates southern staurolite strain stratigraphic structural suggests surfaces Table tectonic temperature texture thickness thrust trend units upper valley West zone
Bibliographic information
| Title | Himalaya: Geological Aspects, Volume 2 Volume 15 of Current trends in geology Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 2 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Publishing House, 2005 |
| ISBN | 8190228986, 9788190228985 |
| Length | 660 pages |
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