Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 52
Thus , the relief on the top of the lower nappe was thrust under the front of the
upper nappe . This nappe character is most conspicuous in partial nappes of the
later thrust phase in the Great Himalaya . These partial nappes formed the main ...
Thus , the relief on the top of the lower nappe was thrust under the front of the
upper nappe . This nappe character is most conspicuous in partial nappes of the
later thrust phase in the Great Himalaya . These partial nappes formed the main ...
Page 83
During the formation of the relief thrusts the zone of the Main Central Thrust was
reactivated alongwith intense rock deformation . INTRODUCTION Geological
research started in the Himalayas 130 years ago . The investigators of these
early ...
During the formation of the relief thrusts the zone of the Main Central Thrust was
reactivated alongwith intense rock deformation . INTRODUCTION Geological
research started in the Himalayas 130 years ago . The investigators of these
early ...
Page 86
The interference of tectonics with the developing relief , however , is not confined
to the Siwalik Zone . In Quaternary times , when a relief was already far advanced
, the latter was disturbed by thrusting . Nappes moved onto adjacent units ...
The interference of tectonics with the developing relief , however , is not confined
to the Siwalik Zone . In Quaternary times , when a relief was already far advanced
, the latter was disturbed by thrusting . Nappes moved onto adjacent units ...
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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