Himalaya: Geological Aspects, Volume 2P. S. Saklani Contributed articles. |
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Page 160
... resulted in the reorientation of axial planes of F , folds ( Fig . 6 ) . In many areas , S , cleavage is curved and folded due to F , superposition ( Fig . 6 ) . The two sets of pucker lineation PL , and PL , are related to F , and F ...
... resulted in the reorientation of axial planes of F , folds ( Fig . 6 ) . In many areas , S , cleavage is curved and folded due to F , superposition ( Fig . 6 ) . The two sets of pucker lineation PL , and PL , are related to F , and F ...
Page 166
... resulted in the formation of regional Chamba - Bharmaur syncline with a core of Kalhel limestone ( Lower Triassic age ) . The reorientation of the meso structures was brought about by the continuation of the movement as shown by the ...
... resulted in the formation of regional Chamba - Bharmaur syncline with a core of Kalhel limestone ( Lower Triassic age ) . The reorientation of the meso structures was brought about by the continuation of the movement as shown by the ...
Page 521
... resulted due to the tendency of these masses to " flow round " the primary bent shape of the collision zone delimited by the southern boundary of Tibet . This was accomplished by shearing parallel to this shape , which was active from ...
... resulted due to the tendency of these masses to " flow round " the primary bent shape of the collision zone delimited by the southern boundary of Tibet . This was accomplished by shearing parallel to this shape , which was active from ...
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