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Page 125
According to NAHA & RAY (1970) the E—W - trending structures belong to first
and second phases of deformation, but Bhattacharya & Niyogi ( 1971 ) regard the
NW—SE-trending structures as belonging to the first and second generations of ...
According to NAHA & RAY (1970) the E—W - trending structures belong to first
and second phases of deformation, but Bhattacharya & Niyogi ( 1971 ) regard the
NW—SE-trending structures as belonging to the first and second generations of ...
Page 177
B. Formation of the F2 folds and the S2 cleavage During the initial stages of
deformation the dip of the listric basement faults was low and the horizontal
movement at the base was transmitted as subvertical with a larger horizontal
component.
B. Formation of the F2 folds and the S2 cleavage During the initial stages of
deformation the dip of the listric basement faults was low and the horizontal
movement at the base was transmitted as subvertical with a larger horizontal
component.
Page 448
RELATION BETWEEN DEFORMATION AND METAMORPHISM The Daling rocks
contain deformational structures of three recognisable generations, and in
general, a strong flattening fabric (Sinha-Roy, l979a). These rocks are also ...
RELATION BETWEEN DEFORMATION AND METAMORPHISM The Daling rocks
contain deformational structures of three recognisable generations, and in
general, a strong flattening fabric (Sinha-Roy, l979a). These rocks are also ...
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Contents
Tectonics and Structure of the Pamirs | 9 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 19 |
Peninsular and Himalayan Precambrian Belts | 31 |
Copyright | |
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Common terms and phrases
Acharyya Alpine Alps associated basement faults basin batholith belt biotite Bordet Central Crystalline collision continental Cretaceous crust crustal deformation deposits Earth Planet earthquakes Eastem Eocene facies field first flow flysch folds foreland formation Gansser Garhwal Geodynamics Geol Geology Geophys geosyncline gneiss Gondwana granite Himalaya Indian plate Indus island arc Jour Karakorum Kashmir Klootwijk Krol Kumaun Ladakh Late Lesser Himalaya limestone lndus Lower magmatic Main Boundary Main Central Thrust margin melange Mesozoic metamorphism Molnar movement nappe Nepal northem occur oceanic ofthe ophiolite orogenic Pakistan Palaeogene palaeomagnetic Palaeozoic Pamir Pande Panjal phase plate tectonics Plateau Precambrian Proterozoic quartzite Quetta Range region rocks rotation Saklani sandstones Saxena schists sedimentary sediments seismicity sequence serpentinite significance Simla Siwalik southem stratigraphic structural subduction Surv suture zone Tectonic Zone Tectonophysics Tertiary Tethyan Tethys thickness Tibetan slab Upper Valdiya volcanics westem
Bibliographic information
| Title | Himalaya: geological aspects Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 15 of Current trends in geology Volume 1 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Author | P. S. Saklani |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Pub. House, 2005 |
| ISBN | 8190228978, 9788190228978 |
| Length | 493 pages |
| Subjects | › › Geology Geology, Structural Metamorphism (Geology) Mountains Science / Earth Sciences / Geology |
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