Himalaya: Geological Aspects, Volume 2Contributed articles. |
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Page 520
In the Kathmandu region some of the ENE - WSW faults have a strike - slip
component ( Stocklin and Bhattarai , 1977 ) . It seems that they occur in a low -
angle ( Riedel - R ) position in relation to the first - order movements along the ...
In the Kathmandu region some of the ENE - WSW faults have a strike - slip
component ( Stocklin and Bhattarai , 1977 ) . It seems that they occur in a low -
angle ( Riedel - R ) position in relation to the first - order movements along the ...
Page 523
First of all , the faults are derived from the regional NNE - SSW or N - S
compression . The bisectrix of the dihedral angle between the faults shows a
tendency to be parallel to the compression . Such a hypothesis of genesis of
these faults is ...
First of all , the faults are derived from the regional NNE - SSW or N - S
compression . The bisectrix of the dihedral angle between the faults shows a
tendency to be parallel to the compression . Such a hypothesis of genesis of
these faults is ...
Page 614
The Ku Ri anticline has been displaced eastwards by later formed ENEWSW
trending Chhiming Ri Fault . Other old structures are the two parallel faults of
Benangung and faults of U Ri , Tsala Ri , and Dechhling . These trend NNW -
SSE ...
The Ku Ri anticline has been displaced eastwards by later formed ENEWSW
trending Chhiming Ri Fault . Other old structures are the two parallel faults of
Benangung and faults of U Ri , Tsala Ri , and Dechhling . These trend NNW -
SSE ...
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Contents
The Central Himalayan Gneisses in Northern Pakistan | 1 |
LowPressure Metamorphism in a Regionally Metamorphic | 39 |
The Buniyar Granite of the Kashmir Himalaya | 61 |
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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 |
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