Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 141
Tanakki Boulder Beds have been found to be equivalent of Blaini Boulder Beds ,
and they are undisputably glacial in character . The Tanakki Boulder Bed in the
Tanol Zone overlies both the Tanols and Hazara Slate ; crinoid bearing ...
Tanakki Boulder Beds have been found to be equivalent of Blaini Boulder Beds ,
and they are undisputably glacial in character . The Tanakki Boulder Bed in the
Tanol Zone overlies both the Tanols and Hazara Slate ; crinoid bearing ...
Page 150
The Carboniferous Chamba and Blaini Tillites indicate that the Himalayan zone
was connected with the Indian subcontinent ; it was situated at that time in the
glacial , near - polar climatic zone of the southern hemisphere , and it drifted
during ...
The Carboniferous Chamba and Blaini Tillites indicate that the Himalayan zone
was connected with the Indian subcontinent ; it was situated at that time in the
glacial , near - polar climatic zone of the southern hemisphere , and it drifted
during ...
Page 287
Late Palaeozoic glaciation Vs. volcanic activity along the Himalayan chain with
special reference to Eastern Himalaya . Himalayan Geol , 3 : 209-230 . Acharyya
, S.K. 1976. On the nature of the Main Boundary Fault in the Daljeeling Sub ...
Late Palaeozoic glaciation Vs. volcanic activity along the Himalayan chain with
special reference to Eastern Himalaya . Himalayan Geol , 3 : 209-230 . Acharyya
, S.K. 1976. On the nature of the Main Boundary Fault in the Daljeeling Sub ...
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Contents
Tectonics and Structure of the Pamirs | 1 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 17 |
Peninsular and Himalayan Precambrian Belts | 31 |
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 existence 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 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