Himalaya: Geological Aspects, Volume 2Contributed articles. |
From inside the book
Results 1-3 of 75
Page 19
No magmatic cumulates have been found in outcrop , but undeformed wherlite
and gabbro pebbles with magmatic structures are frequent in the easternmost
valley . Dikelets of different types are common : dunite occurs in irregular bodies
or ...
No magmatic cumulates have been found in outcrop , but undeformed wherlite
and gabbro pebbles with magmatic structures are frequent in the easternmost
valley . Dikelets of different types are common : dunite occurs in irregular bodies
or ...
Page 151
However , the neotectonic stress field in the Chamba region evaluated by
studying the valley trends and orientation of joints shows north - south
neotectonic stress field . Therefore , the principal compressive stress direction
has changed from ...
However , the neotectonic stress field in the Chamba region evaluated by
studying the valley trends and orientation of joints shows north - south
neotectonic stress field . Therefore , the principal compressive stress direction
has changed from ...
Page 645
STRUCTURAL GEOLOGY OF THE SIYOM VALLEY ARUNACHAL PRADESH
Surendra Singh and A.K. De ABSTRACT The Siyom valley of Arunachal
Himalaya comprises three major tectonic units which from east to west are : ( a )
Nikte ...
STRUCTURAL GEOLOGY OF THE SIYOM VALLEY ARUNACHAL PRADESH
Surendra Singh and A.K. De ABSTRACT The Siyom valley of Arunachal
Himalaya comprises three major tectonic units which from east to west are : ( a )
Nikte ...
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