Himalaya: Geological Aspects, Volume 1Contributed articles. |
From inside the book
Results 1-3 of 89
Page 188
... BETWEEN CONTINENTAL INDO - PAKISTAN AND SOUTH CENTRAL ASIA -
AND PALAEOLATITUDINAL POSITION OF THE COLLISION ZONE The timing of
collision of the Indo - Pakistani subcontinent with southern Asia is disputed .
... BETWEEN CONTINENTAL INDO - PAKISTAN AND SOUTH CENTRAL ASIA -
AND PALAEOLATITUDINAL POSITION OF THE COLLISION ZONE The timing of
collision of the Indo - Pakistani subcontinent with southern Asia is disputed .
Page 214
... far to the south of the palaeoposition of the former southern boundary of south
central Asia , following Powell's ( 1979 ) suggestion that this boundary is
represented by the eastwards continuation of the Zagros - Makran convergence
zone .
... far to the south of the palaeoposition of the former southern boundary of south
central Asia , following Powell's ( 1979 ) suggestion that this boundary is
represented by the eastwards continuation of the Zagros - Makran convergence
zone .
Page 215
For palaeomagnetically studied areas situated directly north of the Indus -
Tsangpo suture zone ( i.e. the Eastern Hindu Kush , Ladakh and southern Tibet )
have been compared in Figure 10 and Table VIII . The observed palaeolatitudes
for ...
For palaeomagnetically studied areas situated directly north of the Indus -
Tsangpo suture zone ( i.e. the Eastern Hindu Kush , Ladakh and southern Tibet )
have been compared in Figure 10 and Table VIII . The observed palaeolatitudes
for ...
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