Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 368
... geochronological studies in this region indicate that the age of high grade
metamorphism in the older rocks ( Jutogh / Almora - Schists ) is related to
migmatization which followed Fd2 - fotding and ranged from 42 + 3 to 59 + 3 m.y.
( Pande ...
... geochronological studies in this region indicate that the age of high grade
metamorphism in the older rocks ( Jutogh / Almora - Schists ) is related to
migmatization which followed Fd2 - fotding and ranged from 42 + 3 to 59 + 3 m.y.
( Pande ...
Page 371
... in texture , structure and mineral relations ( Pande , 1956 ; Pande et al , 1963 ) .
In general , the rocks are crystalloblastic , highly foliated ( three to four sets of
cleavage : Mahajan and Pande , 1974 ) and medium to coarse grained ( Figs .
... in texture , structure and mineral relations ( Pande , 1956 ; Pande et al , 1963 ) .
In general , the rocks are crystalloblastic , highly foliated ( three to four sets of
cleavage : Mahajan and Pande , 1974 ) and medium to coarse grained ( Figs .
Page 382
Pande ( 1966 ) stressed the emergence of Central Crystalline Axis ' as a result of
remobilisation of the basement at depth ( Fig 4a ) during Caledonian orogenesis .
The emergence of Central Crystalline Axis ( coastal ridee ) synchronous with ...
Pande ( 1966 ) stressed the emergence of Central Crystalline Axis ' as a result of
remobilisation of the basement at depth ( Fig 4a ) during Caledonian orogenesis .
The emergence of Central Crystalline Axis ( coastal ridee ) synchronous with ...
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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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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