Himalaya: Geological Aspects, Volume 2P. S. Saklani Contributed articles. |
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Page 388
... Chail units . This follows from the fact that the " Krol Nappe " cannot be traced toward the N , into a position higher than the Chail units . There is no root zone of the hypothetical " Krol Nappe " between the Chail Nappes and the ...
... Chail units . This follows from the fact that the " Krol Nappe " cannot be traced toward the N , into a position higher than the Chail units . There is no root zone of the hypothetical " Krol Nappe " between the Chail Nappes and the ...
Page 389
... Chail Nappes ; but in the lowest , parautochthonous units , which were deposited in the southernmost parts of the zone characterized by Chail sedimentation , the alteration becomes faint and almost imperceptible . Towards the N , to the ...
... Chail Nappes ; but in the lowest , parautochthonous units , which were deposited in the southernmost parts of the zone characterized by Chail sedimentation , the alteration becomes faint and almost imperceptible . Towards the N , to the ...
Page 390
... Chail Nappes further east , but I use the term Tanol Zone , because it is doubtful whether it forms a real nappe or is just parautochthonous . The Tanol Zone may be traced around the NW - Syntaxis and joins up with the phyllite ...
... Chail Nappes further east , but I use the term Tanol Zone , because it is doubtful whether it forms a real nappe or is just parautochthonous . The Tanol Zone may be traced around the NW - Syntaxis and joins up with the phyllite ...
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