Himalaya: Geological Aspects, Volume 2Contributed articles. |
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Page 306
This can be illustrated by a restoration of the Krol sheet into its pre - movement
position in the basin . During the active slip on the basal thrust - or slide - of the
Munsiari sheet a lenticular horse , measuring over 100 km along strike and < 9km
in ...
This can be illustrated by a restoration of the Krol sheet into its pre - movement
position in the basin . During the active slip on the basal thrust - or slide - of the
Munsiari sheet a lenticular horse , measuring over 100 km along strike and < 9km
in ...
Page 308
This they regard as being earlier than the Krol thrust . A second episode
produced asymmetric folds accompanied by axial plane cleavage and the author
links this folding with the translation on the Krol thrust . Rather similar folding /
thrusting ...
This they regard as being earlier than the Krol thrust . A second episode
produced asymmetric folds accompanied by axial plane cleavage and the author
links this folding with the translation on the Krol thrust . Rather similar folding /
thrusting ...
Page 313
TECTONIC UNITS Between the Krol and Vaikrita thrusts the Lesser Himalayan
subprovince is built up of three major thrust sheets or nappes ( with their klippen )
covering the autochthon discernible in windows . Each of these units has its own
...
TECTONIC UNITS Between the Krol and Vaikrita thrusts the Lesser Himalayan
subprovince is built up of three major thrust sheets or nappes ( with their klippen )
covering the autochthon discernible in windows . Each of these units has its own
...
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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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