Himalaya: Geological Aspects, Volume 2Contributed articles. |
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Page 94
Hoschek ( in Winkler , 1967 ) , on the basis of experimental data , evaluated the
temperature for this reaction to be 540 ° C # 15 ° C at 4000 bars and 560 ° C + 15
° C at 7000 bars of H2O pressure and similar pressure could be visualized for ...
Hoschek ( in Winkler , 1967 ) , on the basis of experimental data , evaluated the
temperature for this reaction to be 540 ° C # 15 ° C at 4000 bars and 560 ° C + 15
° C at 7000 bars of H2O pressure and similar pressure could be visualized for ...
Page 548
( 2 ) The product and reactant assemblages of the reaction ( 2 ) are plotted on the
map ( Fig . 14 ) similar to the garnet isograd ( Fig . 13 ) . There is almost complete
exclusion between the reactants and the product except near the isograd where ...
( 2 ) The product and reactant assemblages of the reaction ( 2 ) are plotted on the
map ( Fig . 14 ) similar to the garnet isograd ( Fig . 13 ) . There is almost complete
exclusion between the reactants and the product except near the isograd where ...
Page 550
The modal decrease of kyanite and textural evidence of sillimanite fringing
kyanite are supporting evidences of the reaction ( 4 ) . In Figure 16 the reactant
and product assemblages of the reaction ( 4 ) are plotted . Kyanite persists on the
...
The modal decrease of kyanite and textural evidence of sillimanite fringing
kyanite are supporting evidences of the reaction ( 4 ) . In Figure 16 the reactant
and product assemblages of the reaction ( 4 ) are plotted . Kyanite persists on the
...
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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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