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Page 317
Cornplexly folded and severely deformed, particularly in the proximity of the
thrust planes, the autochthonous zone erdribits series of tight asymmetrical to
overtumed and locally isoclinal folds, many of them being split up by faults or
thrusts ...
Cornplexly folded and severely deformed, particularly in the proximity of the
thrust planes, the autochthonous zone erdribits series of tight asymmetrical to
overtumed and locally isoclinal folds, many of them being split up by faults or
thrusts ...
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 Northem Pakistan | 1 |
Ductile Shearing in Peridotites of Spongtang Nappe Ladakh | 27 |
LowPressure Metamorphism in a Regionally Metamorphic | 39 |
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Almora amphibolite andalusite assemblages augen gneiss axes axial plane bedding belt Berinag Bhutan biotite Buxa Central Crystallines Chail Chail Nappes chlorite Chomolongma crenulation cleavage defined defonnation developed eastem F2 folds fabric facies faults feldspar field first flattening foliation Fonnation Formation fractures gamet Gansser Garhwal Garhwal Himalaya garnet Geol Geology girdle gneiss Gondwana grade grains granite gneiss Group Himalaya isograd Jour Jutogh Khola Khumbu Krol Kumaun kyanite Lesser Himalaya limestone lithological lower Main Central Thrust Makalu metasediments mica schist micaceous migmatites mineral lineation muscovite mylonitic nappe Nepal northem occur orientation parallel pattem pelitic Phaplu phase of deformation phyllites plagioclase porphyroblasts Pradesh Precambrian quartz quartzite reaction rocks Saklani schist schistosity sedimentary sediments sequence sericite shear significant sillimanite Simla Siwalik Siyom slates southem staurolite stratigraphic strike-slip structural Surv syncline tectonic texture Thimpu thrust sheet thrust zone trend upper Valdiya valley westem
Bibliographic information
| Title | Himalaya: geological aspects Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 15 of Current trends in geology Volume 2 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Author | P. S. Saklani |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Pub. House, 2005 |
| ISBN | 8190228986, 9788190228985 |
| Length | 660 pages |
| Subjects | › › Geology Geology, Structural Metamorphism (Geology) Science / Earth Sciences / Geology |
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