Himalaya: Geological Aspects, Volume 2Contributed articles. |
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Page 182
The angle between S2 (AA') and S2 surface (CD) is 70°. The S2 and S 2 surfaces
though not very prominent can be recognised. Pattern No. 2." Location 1 '/1
furlongs from B.D.O. towards Khabli bazar. The geometrical feature of this pattern
...
The angle between S2 (AA') and S2 surface (CD) is 70°. The S2 and S 2 surfaces
though not very prominent can be recognised. Pattern No. 2." Location 1 '/1
furlongs from B.D.O. towards Khabli bazar. The geometrical feature of this pattern
...
Page 182
The boudins make an angle with the main foliation . ... The rock dips 15o due S
60 ° E . As drawn in Figure 7 , there are two more discontinuities AA ' and BB '
which cut across the foliation S , at low angles besides the S , surface ( marked
by ...
The boudins make an angle with the main foliation . ... The rock dips 15o due S
60 ° E . As drawn in Figure 7 , there are two more discontinuities AA ' and BB '
which cut across the foliation S , at low angles besides the S , surface ( marked
by ...
Page 507
1 - foliation in downthrown side of thrust , 2 - S , fractures of the Riedel type in low
- angle position to the thrust , 3 - thrust surface ( T ) , 4 - foliation in upthrown side
of thrust , 5 - intersection of S , fractures with thrust surface ( 0 ) , 6 - trace of ...
1 - foliation in downthrown side of thrust , 2 - S , fractures of the Riedel type in low
- angle position to the thrust , 3 - thrust surface ( T ) , 4 - foliation in upthrown side
of thrust , 5 - intersection of S , fractures with thrust surface ( 0 ) , 6 - trace of ...
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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