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Page 71
the mode of subduction are interrelated and therefore the Marina-type subduction
characterised by extensional backarc stress have less massive island arc with
abundant basaltic volcanic pile overlying the oceanic basement crust.
the mode of subduction are interrelated and therefore the Marina-type subduction
characterised by extensional backarc stress have less massive island arc with
abundant basaltic volcanic pile overlying the oceanic basement crust.
Page 104
According to Gansser (I964), Biq (1968, 1971), and Dewey and Bird (1970), the
total disappearance of the onetime existing eugeosynclinal sequence from the
Himalayan region is due to its complete subduction to subcrustal depth at the
lndus ...
According to Gansser (I964), Biq (1968, 1971), and Dewey and Bird (1970), the
total disappearance of the onetime existing eugeosynclinal sequence from the
Himalayan region is due to its complete subduction to subcrustal depth at the
lndus ...
Page 111
Garhwal Nappe carved into the Great Himalaya and subducted beneath which
has been a 100-km-wide segment of the lndian Shield with a sediment coat of the
Gondwanic fashion. However, owing to the equal density of the downgoing and ...
Garhwal Nappe carved into the Great Himalaya and subducted beneath which
has been a 100-km-wide segment of the lndian Shield with a sediment coat of the
Gondwanic fashion. However, owing to the equal density of the downgoing and ...
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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 |
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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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