Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 199
The appreciable change in palaeomagnetic directions throughout these late
Palaeozoic formation is also visible in recently obtained data for the late
Palaeozoic of Kashmir . It broadly reflects the large drift of Gondwanaland over
the south ...
The appreciable change in palaeomagnetic directions throughout these late
Palaeozoic formation is also visible in recently obtained data for the late
Palaeozoic of Kashmir . It broadly reflects the large drift of Gondwanaland over
the south ...
Page 338
In Kashmir no thrust equivalent in magnitude or extension to the Main Central
Thrust exists . The Main Boundary Fault itself is split into two major faults viz . the
so called Main Boundary Fault ( Middlemiss , 1919 ; Wadia , 1928 ; Jammu Fault
of ...
In Kashmir no thrust equivalent in magnitude or extension to the Main Central
Thrust exists . The Main Boundary Fault itself is split into two major faults viz . the
so called Main Boundary Fault ( Middlemiss , 1919 ; Wadia , 1928 ; Jammu Fault
of ...
Page 344
Obviously , while Cambrian to Carboniferous sequence of eastern Kashmir is
similar to that of the “ Tethyan ” zone , Permo - Carboniferous facies in the whole
of Kashmir is identical to that of Lesser Himalayan zone . Viewed in this
perspective ...
Obviously , while Cambrian to Carboniferous sequence of eastern Kashmir is
similar to that of the “ Tethyan ” zone , Permo - Carboniferous facies in the whole
of Kashmir is identical to that of Lesser Himalayan zone . Viewed in this
perspective ...
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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