Himalaya: Geological Aspects, Volume 2Contributed articles. |
From inside the book
Results 1-3 of 76
Page 383
This sequence of tectonic units is generally known as the inverse metamorphism
of the Himalaya . Also within the Chail Nappe system the grade of alteration
increases upwards and towards the root zone . It is shown that the Chail Nappe ...
This sequence of tectonic units is generally known as the inverse metamorphism
of the Himalaya . Also within the Chail Nappe system the grade of alteration
increases upwards and towards the root zone . It is shown that the Chail Nappe ...
Page 451
Tectonic Unit Lithostratigraphy Mahabharat Klippe Tethyan Series Khumbu
Nappe Khumbu Migmatite Rasuwa T ) ( Khumbu T ) Higher Crystalline Sheet
Himalayan Gneiss ( Sarung T ) Khali Khola Schist Lower Crystalline Sheet
Phaplu ...
Tectonic Unit Lithostratigraphy Mahabharat Klippe Tethyan Series Khumbu
Nappe Khumbu Migmatite Rasuwa T ) ( Khumbu T ) Higher Crystalline Sheet
Himalayan Gneiss ( Sarung T ) Khali Khola Schist Lower Crystalline Sheet
Phaplu ...
Page 576
Syn - tectonic granite emplacement at high structural levels ( Auden , 1935 ;
Misch ; 1949 ) along prominent dislocations zones together with frictional heating
along these zones ( Sinha Roy , 1975a ) appear to meet the demands of
structural ...
Syn - tectonic granite emplacement at high structural levels ( Auden , 1935 ;
Misch ; 1949 ) along prominent dislocations zones together with frictional heating
along these zones ( Sinha Roy , 1975a ) appear to meet the demands of
structural ...
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
Bibliographic information
| Title | Himalaya: Geological Aspects, Volume 2 Volume 15 of Current trends in geology Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 2 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Publishing House, 2005 |
| ISBN | 8190228986, 9788190228985 |
| Length | 660 pages |
| Export Citation | BiBTeX EndNote RefMan |