Himalaya: Geological Aspects, Volume 2P. S. Saklani Contributed articles. |
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Page 20
... flattening plane of the minerals ( Nicolas et al . , 1972 ; Nicolas and Jackson , 1972 ) . In the case of progressive simple shear the glide plane is oblique in respect to the flattening plane , but with increasing intensity of the ...
... flattening plane of the minerals ( Nicolas et al . , 1972 ; Nicolas and Jackson , 1972 ) . In the case of progressive simple shear the glide plane is oblique in respect to the flattening plane , but with increasing intensity of the ...
Page 575
... flattening strain and strong extensions in the thrust zone , the strain symmetry appears to have changed from flattening type outside to constrictional type within the thrust - zone . This explains the stretching mineral lineation , an ...
... flattening strain and strong extensions in the thrust zone , the strain symmetry appears to have changed from flattening type outside to constrictional type within the thrust - zone . This explains the stretching mineral lineation , an ...
Page 580
... Daling rocks and the Lingtse Gneiss . This indicates that F , folds are variably flattened , and that the superimposed flattening strain is variable in space , being related to thrusting . a 15 cm art ( i ) SO- b 8cm 580 S. Sinha Roy.
... Daling rocks and the Lingtse Gneiss . This indicates that F , folds are variably flattened , and that the superimposed flattening strain is variable in space , being related to thrusting . a 15 cm art ( i ) SO- b 8cm 580 S. Sinha Roy.
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