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Page 162
The plots of S , surface for the Chamba syncline have been shown in figure 74.
The stereoplot reveal one maxima suggesting either it could be one limb of the
fold or the fold geometry is such that both the limbs dip in the same direction .
The plots of S , surface for the Chamba syncline have been shown in figure 74.
The stereoplot reveal one maxima suggesting either it could be one limb of the
fold or the fold geometry is such that both the limbs dip in the same direction .
Page 182
7) is also seen in Figure 8 showing the plane dipping at 80° due NNW. 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
...
7) is also seen in Figure 8 showing the plane dipping at 80° due NNW. 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
...
Page 484
The deformation associated with the Phaplu thrust - movements is illustrated in
Figure 24. The attitude of the lineations and asymmetrical Fp , folds with
southward vergence indicate the direction of tectonic transport varied from N /
NNE to S ...
The deformation associated with the Phaplu thrust - movements is illustrated in
Figure 24. The attitude of the lineations and asymmetrical Fp , folds with
southward vergence indicate the direction of tectonic transport varied from N /
NNE to S ...
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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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