Himalaya: Geological Aspects, Volume 1Contributed articles. |
From inside the book
Results 1-3 of 72
Page 192
Crawford ( 1974c ) suggested that the Salt Range - Potwar Plateau unit was
formerly in line with the main Himalayan front and ... These samples from 13
lithological units ( Table II ) range in age from late Palaeozoic to early Tertiary ,
i.e. in the ...
Crawford ( 1974c ) suggested that the Salt Range - Potwar Plateau unit was
formerly in line with the main Himalayan front and ... These samples from 13
lithological units ( Table II ) range in age from late Palaeozoic to early Tertiary ,
i.e. in the ...
Page 351
Although each of the major nappes or thrust sheets , has a complex history
during transport , the whole of the unit can be ... This paper stresses the
importance of thrust tectonics in the present disposition of the main lithostructural
units .
Although each of the major nappes or thrust sheets , has a complex history
during transport , the whole of the unit can be ... This paper stresses the
importance of thrust tectonics in the present disposition of the main lithostructural
units .
Page 427
( c ) The pyroxene and platy - gneiss ( unit “ b ” ) of Tibetan slab should be a
synclinal scar , causing the sedimentary series ... There are several facts which
do not favour such an interpretation : the non - symmetrical succession of units in
the ...
( c ) The pyroxene and platy - gneiss ( unit “ b ” ) of Tibetan slab should be a
synclinal scar , causing the sedimentary series ... There are several facts which
do not favour such an interpretation : the non - symmetrical succession of units in
the ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
8 other sections not shown
Other editions - View all
Common terms and phrases
active Asia associated base basement basic basin beds belt biotite blocks Boundary Central collision complex consists continental continuous Cretaceous crust crystalline deformation deposits direction early earthquakes east eastern Eocene et al evolution extension facies faults Figure folds followed formation formed Gansser Garhwal Geol Geology gneiss grade granite Group Higher Himalaya Indian Indian plate indicate Indus initial island Jour Kashmir Ladakh Late Lesser levels limestone Lower magmatic major margin metamorphism Middle mountain movement nappe nature Nepal northern observed occur oceanic ophiolite origin orogenic Pakistan palaeomagnetic Palaeozoic Pande phase plate possible Precambrian present Range region represent rocks rotation sampled sandstones schists sedimentary sediments seismicity sequence Shield similar southern structural studies subduction suggested suture Table tectonic Tertiary Tethyan thickness thrust Tibetan trend units Upper valley volcanics western zone