Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 125
According to NAHA & RAY ( 1970 ) the E - W - trending structures belong to first
and second phases of deformation , but Bhattacharya & Niyogi ( 1971 ) regard
the NW - SE - trending structures as belonging to the first and second
generations ...
According to NAHA & RAY ( 1970 ) the E - W - trending structures belong to first
and second phases of deformation , but Bhattacharya & Niyogi ( 1971 ) regard
the NW - SE - trending structures as belonging to the first and second
generations ...
Page 216
Molnar and Tapponnier noted : ( a ) that the indentation in the Hindu Kush -
Pamir - Karakorum zone accords at best with a wide angle wedge shaped
indenter , and ( b ) that deformation over vast areas of southern Asia reflects the
effects of a ...
Molnar and Tapponnier noted : ( a ) that the indentation in the Hindu Kush -
Pamir - Karakorum zone accords at best with a wide angle wedge shaped
indenter , and ( b ) that deformation over vast areas of southern Asia reflects the
effects of a ...
Page 448
RELATION BETWEEN DEFORMATION AND METAMORPHISM The Daling rocks
contain deformational structures of three recognisable generations , and in
general , a strong flattening fabric ( Sinha - Roy , 1979a ) . These rocks are also ...
RELATION BETWEEN DEFORMATION AND METAMORPHISM The Daling rocks
contain deformational structures of three recognisable generations , and in
general , a strong flattening fabric ( Sinha - Roy , 1979a ) . These rocks are also ...
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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