Himalaya: Geological Aspects, Volume 2Contributed articles. |
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Page 173
The eastern limb of this Vshaped structure trends independently as compared to
the western limb . The western limb has a varied trend from NW - SE to E - W
whereas the eastern limb trends NE - SW constantly . These trends might have
been ...
The eastern limb of this Vshaped structure trends independently as compared to
the western limb . The western limb has a varied trend from NW - SE to E - W
whereas the eastern limb trends NE - SW constantly . These trends might have
been ...
Page 180
TRANSVERSE STRUCTURES The NE - SW trend of the Bhankoli - Barkot
formation is a very characteristic transverse structure as against the NW - SE
trending Main Central Thrust which follows the Himalayan trend . The thrust cuts
off the ...
TRANSVERSE STRUCTURES The NE - SW trend of the Bhankoli - Barkot
formation is a very characteristic transverse structure as against the NW - SE
trending Main Central Thrust which follows the Himalayan trend . The thrust cuts
off the ...
Page 187
The axes of folds near the tectonic contact of Sauli and Nawagaon Formations
trend N 10 ° E – S 10 ° W . The folds in the limestones of Sauli Formation
exposed on the western limb side of Nawagaon synform show their axes
generally ...
The axes of folds near the tectonic contact of Sauli and Nawagaon Formations
trend N 10 ° E – S 10 ° W . The folds in the limestones of Sauli Formation
exposed on the western limb side of Nawagaon synform show their axes
generally ...
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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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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