Himalaya: Geological Aspects, Volume 2Contributed articles. |
From inside the book
Results 1-3 of 75
Page 15
In the central Ladakh , all the authors recognize different lithostructural units
showing their regional trend ( NW - SE ) parallel to the “ Indus suture ” . To the
south of it , the Spongtang klippe ( the Shillakong ophiolite nappe of Srikantia
and ...
In the central Ladakh , all the authors recognize different lithostructural units
showing their regional trend ( NW - SE ) parallel to the “ Indus suture ” . To the
south of it , the Spongtang klippe ( the Shillakong ophiolite nappe of Srikantia
and ...
Page 388
also is parautochthnous and always had a position S of the deposition area of the
Chail units . This follows from the fact that the “ Krol Nappe ” cannot be traced
toward the N , into a position higher than the Chail units . There is no root zone of
...
also is parautochthnous and always had a position S of the deposition area of the
Chail units . This follows from the fact that the “ Krol Nappe ” cannot be traced
toward the N , into a position higher than the Chail units . There is no root zone of
...
Page 391
The lowest unit is exposed in the core of the Tons anticlinorium and consists of a
sequence of Chail ( Valdiya's Rautgara Fm . ) and thick Deoban carbonates . The
lower Chail units abut against the Simla Slates of Chakrata along a steep or ...
The lowest unit is exposed in the core of the Tons anticlinorium and consists of a
sequence of Chail ( Valdiya's Rautgara Fm . ) and thick Deoban carbonates . The
lower Chail units abut against the Simla Slates of Chakrata along a steep or ...
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 |