Himalaya: Geological Aspects, Volume 2P. S. Saklani Contributed articles. |
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Page 306
... Berinag thrust has been equated with the Krol by Valdiya ( 1980 , 1981 ) and the close proximity of the trailing edge of the Krol to the leading edge of the Berinag makes this a reasonable view . Valdiya notes however that the Berinag ...
... Berinag thrust has been equated with the Krol by Valdiya ( 1980 , 1981 ) and the close proximity of the trailing edge of the Krol to the leading edge of the Berinag makes this a reasonable view . Valdiya notes however that the Berinag ...
Page 307
... Berinag sheet must be explained by post - thrust folding and erosion ( Fig . 3C ) . This interpretation ( ' Eroded ramp model ' ) is plausible if perhaps somewhat contrived . But it does not account for the ? duplexes involving Nagthat ...
... Berinag sheet must be explained by post - thrust folding and erosion ( Fig . 3C ) . This interpretation ( ' Eroded ramp model ' ) is plausible if perhaps somewhat contrived . But it does not account for the ? duplexes involving Nagthat ...
Page 315
... Berinag succession is apparently conformable in many places , but recent studies clearly demonstrate that a thrust plane separates the Berinag from the underlying formations ( Valdiya , 1968 , 1973 ; Saklani .1971 , 1972 ; Jain , 1971 ...
... Berinag succession is apparently conformable in many places , but recent studies clearly demonstrate that a thrust plane separates the Berinag from the underlying formations ( Valdiya , 1968 , 1973 ; Saklani .1971 , 1972 ; Jain , 1971 ...
Contents
The Central Himalayan Gneisses in Northern Pakistan | 1 |
LowPressure Metamorphism in a Regionally Metamorphic | 49 |
The Aureole Zone and Metasediments of Dhauladhar Chaori Khas H P | 75 |
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Almora amphibolite andalusite anticline assemblages augen gneiss axes axial plane axis Barun bedding belt Berinag Bhutan biotite Buxa Central Crystallines Chail Chail Nappes chlorite Chomolongma crenulation cleavage Darjeeling developed diagram eastern fabric facies faults feldspar folds foliation Formation fractures Fuchs Gansser Garhwal Garhwal Himalaya garnet Geol Geology girdle gneiss Gondwana grade grains granite gneiss Group Himalaya India isograd Jour Jutogh Khola Khumbu Kumaun kyanite Lesser Himalaya limestone lithological lower Main Central Thrust Makalu Massif mesoscopic metasediments mica schist micaceous migmatites mineral lineation muscovite mylonitic nappe Nepal occur orientation parallel pelitic Phaplu phase of deformation phyllites plagioclase porphyroblasts Pradesh Precambrian quartz quartzite reaction regional metamorphism rocks S₂ Saklani schist schistosity sedimentary sediments sequence sericite shear sillimanite Simla Siwalik Siyom slates staurolite stratigraphic strike-slip structural Surv syncline tectonic temperature Tethyan texture Thimpu thrust sheet thrust zone tourmaline trend upper Vaikrita Valdiya valley