Himalaya: Geological Aspects, Volume 2P. S. Saklani Contributed articles. |
From inside the book
Results 1-3 of 71
Page 173
... trends independently as compared to the western limb . The western limb has a varied trend from NW - SE to E - W whereas the eastern limb trends NE - SW constantly . These trends might have been developed independent of each other ...
... trends independently as compared to the western limb . The western limb has a varied trend from NW - SE to E - W whereas the eastern limb trends NE - SW constantly . These trends might have been developed independent of each other ...
Page 180
... trends make an angle of about 30 ° with each other ; the Himalayan trend superimposing upon the transverse structure . The axis of the main syncline i.e. the Nawagaon synform also trends roughly N - S as against the Himalayan NNW - SSE ...
... trends make an angle of about 30 ° with each other ; the Himalayan trend superimposing upon the transverse structure . The axis of the main syncline i.e. the Nawagaon synform also trends roughly N - S as against the Himalayan NNW - SSE ...
Page 187
... trend is N20 ° E - S 20 ° W. The lineation occurs at 50 ° angle to the foliation . However , variation in the trend of this lineation is from N - S to NNW - SSE or NNE SSW . There are a few folds which show their axes trending E - W ( 1 ...
... trend is N20 ° E - S 20 ° W. The lineation occurs at 50 ° angle to the foliation . However , variation in the trend of this lineation is from N - S to NNW - SSE or NNE SSW . There are a few folds which show their axes trending E - W ( 1 ...
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 |
Copyright | |
9 other sections not shown
Other editions - View all
Common terms and phrases
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