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Page 246
TABLE - II Table showing relation between deformation and development of
structural elements dan Lansdowne area ... Axial plane schistosity is schistosity
marked by prefer developed mostly by comprered orientation of ( 001 ) clea ssion
...
TABLE - II Table showing relation between deformation and development of
structural elements dan Lansdowne area ... Axial plane schistosity is schistosity
marked by prefer developed mostly by comprered orientation of ( 001 ) clea ssion
...
Page 261
( 2 ) During the development of L , pucker lineation on S , by convergent
movement along the direction of tectonic ... ( 3 ) The younger puckers L , oblique
or subnormal to L , or Ls have been developed during F , phase of deformation
with a ...
( 2 ) During the development of L , pucker lineation on S , by convergent
movement along the direction of tectonic ... ( 3 ) The younger puckers L , oblique
or subnormal to L , or Ls have been developed during F , phase of deformation
with a ...
Page 288
Thus it is concluded that in the initial stages of D , deformation tight isoclinal folds
( F , ) developed on bedding plane ( S , ) on mesoscopic scale . With the
development of F , folds prominent penetrative axial plane foliation ( S2 )
developed ...
Thus it is concluded that in the initial stages of D , deformation tight isoclinal folds
( F , ) developed on bedding plane ( S , ) on mesoscopic scale . With the
development of F , folds prominent penetrative axial plane foliation ( S2 )
developed ...
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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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