Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 340
The sequence is fossiliferous from Middle Ordovician onwards ( Shah , 1972 ) .
Devonian - Carboniferous sequence , consisting of Muth Quartzite - Syringothyris
Limestone - Fenestella Shale , is well developed in the Kotsu anticline and fairly
...
The sequence is fossiliferous from Middle Ordovician onwards ( Shah , 1972 ) .
Devonian - Carboniferous sequence , consisting of Muth Quartzite - Syringothyris
Limestone - Fenestella Shale , is well developed in the Kotsu anticline and fairly
...
Page 341
Poonch - Pir Panjal belt represents a complete change in the Palaeozoic facies ,
so much so that Wadia ( 1328 ) grouped most of the Palaeozoic sequence into
his Pre - cambrian Dogra Slate and later partly into Salkhala ( Wadia , 1934 ) on ...
Poonch - Pir Panjal belt represents a complete change in the Palaeozoic facies ,
so much so that Wadia ( 1328 ) grouped most of the Palaeozoic sequence into
his Pre - cambrian Dogra Slate and later partly into Salkhala ( Wadia , 1934 ) on ...
Page 444
The parautochthonous Palaeozoic - Mesozoic sedimentary rock sequences of
the Lower Himalaya are weakly ... One of the major problems of metamorphism of
these rocks is the inverted metamorphic sequence , i.e. , the feature of higher ...
The parautochthonous Palaeozoic - Mesozoic sedimentary rock sequences of
the Lower Himalaya are weakly ... One of the major problems of metamorphism of
these rocks is the inverted metamorphic sequence , i.e. , the feature of higher ...
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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