Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 92
Thus the MCT is no more active as an extensive thrust directly forming the relief
gap between the Higher and Lower Himalaya . Although knick points of the major
rivers axe located approximately along the MCT , any concrete evidence of ...
Thus the MCT is no more active as an extensive thrust directly forming the relief
gap between the Higher and Lower Himalaya . Although knick points of the major
rivers axe located approximately along the MCT , any concrete evidence of ...
Page 433
... D.Krumenacher , F.A. Kingery , A.M. Basett , H.F. Layne ABSTRACT K / Ar age
determinations and study of lineations and foliations of rocks of the Higher and
Lower Himalaya lead to a complex picture of the Himalayan metamorphism .
... D.Krumenacher , F.A. Kingery , A.M. Basett , H.F. Layne ABSTRACT K / Ar age
determinations and study of lineations and foliations of rocks of the Higher and
Lower Himalaya lead to a complex picture of the Himalayan metamorphism .
Page 441
LINEATION AND FOLIATION MEASUREMENTS OF ROCKS OF THE HIGHER
HIMALAYA AND THE KATHMANDU NAPPE ( Figs . I to 4 ) Higher Himalaya :
The measurements were performed in all kinds of rocks from the Dudh Kosi
Valley .
LINEATION AND FOLIATION MEASUREMENTS OF ROCKS OF THE HIGHER
HIMALAYA AND THE KATHMANDU NAPPE ( Figs . I to 4 ) Higher Himalaya :
The measurements were performed in all kinds of rocks from the Dudh Kosi
Valley .
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Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
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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