Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 242
Similar events , with an average recurrence time of about 200 years ( Sieh ,
1978a and b ) , have occurred in the past on the same portion of the San Andreas
fault . It is not clear whether the oblique portion of the Chaman fault has
experienced ...
Similar events , with an average recurrence time of about 200 years ( Sieh ,
1978a and b ) , have occurred in the past on the same portion of the San Andreas
fault . It is not clear whether the oblique portion of the Chaman fault has
experienced ...
Page 281
Contemporaneous and similar volcanics occur in the Lesser Himalayan frontal
belt in Tansen area , Nepal ( Sakai , 1983 ) , where the volcanics containing well
preserved Upper Gondwana plant remains unconformably overlie the Late ...
Contemporaneous and similar volcanics occur in the Lesser Himalayan frontal
belt in Tansen area , Nepal ( Sakai , 1983 ) , where the volcanics containing well
preserved Upper Gondwana plant remains unconformably overlie the Late ...
Page 456
A similar metamorphic relationship is likely in the high - temperature
metamorphism exhibited in the Nanga Parbat region ( Turner , 1968 ) . Unlike the
Eastern Alps , however , the highest metamorphic grade of the Himalayan rocks
is realised ...
A similar metamorphic relationship is likely in the high - temperature
metamorphism exhibited in the Nanga Parbat region ( Turner , 1968 ) . Unlike the
Eastern Alps , however , the highest metamorphic grade of the Himalayan rocks
is realised ...
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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