Himalaya: Geological Aspects, Volume 2Contributed articles. |
From inside the book
Results 1-3 of 61
Page 316
The Muliagaon gneiss of the Budhakedar area is a Ramgarh element , and does
not belong to the socalled “ Central Crystallines ” ( root of Almora nappe ) as
suggested by Saklani ( 1972 ) . The Purola Schuppen Zone extends from
Dharasu ...
The Muliagaon gneiss of the Budhakedar area is a Ramgarh element , and does
not belong to the socalled “ Central Crystallines ” ( root of Almora nappe ) as
suggested by Saklani ( 1972 ) . The Purola Schuppen Zone extends from
Dharasu ...
Page 359
This pattern is noted in slaty quartzite in juxtaposition with the North Almora
Thrust . 4. Diagram with two , weak crossed - girdles intersecting in ' ab'plane with
strong maximum concentration inclined by 45 to ' a ' . DISCUSSION As
mentioned ...
This pattern is noted in slaty quartzite in juxtaposition with the North Almora
Thrust . 4. Diagram with two , weak crossed - girdles intersecting in ' ab'plane with
strong maximum concentration inclined by 45 to ' a ' . DISCUSSION As
mentioned ...
Page 360
An analysis of the mesoscopic structures indicates that the deformational
histories of the rocks of both the Badolisera - Pithoragarh Zone and the Almora
Crystalline Mass are largely comparable though there are minor differences .
An analysis of the mesoscopic structures indicates that the deformational
histories of the rocks of both the Badolisera - Pithoragarh Zone and the Almora
Crystalline Mass are largely comparable though there are minor differences .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
The Central Himalayan Gneisses in Northern Pakistan | 1 |
LowPressure Metamorphism in a Regionally Metamorphic | 39 |
The Buniyar Granite of the Kashmir Himalaya | 61 |
Copyright | |
10 other sections not shown
Other editions - View all
Common terms and phrases
Almora angle appears assemblages associated augen axes axial axis bands base bedding belt biotite boundary Chail chlorite cleavage composition consists contain continuous crenulation crystalline deformation developed diagram direction District eastern exposed fabric facies faults folds foliation Formation formed fractures Garhwal garnet Geol Geology girdle gneiss grade grains granite Group higher Himalaya inclusions increase India indicate isograd Jour Jutogh Krol Kumaun kyanite Lesser Himalaya limestone lineation lower Main Central major metamorphism mica migmatites mineral movement muscovite mylonitic nappe Nepal observed occur orientation parallel pelitic phase phyllites plagioclase plane porphyroblasts present pressure quartz quartzite range reaction region relief represented result rocks Saklani schist schistosity sequence sericite sets shear sheet sillimanite similar Siwalik slates southern staurolite strain stratigraphic structural suggests surfaces Table tectonic temperature texture thickness thrust trend units upper valley West zone