Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 235
Fault - plane solutions indicate that it is a zone of thrust faulting that dips to the
northeast ( Armbruster et al . , 1978 ; Pennington , 1979 ) . The slip - direction is
approximately perpendicular to the strike of the IKSZ . This is similar to
observations ...
Fault - plane solutions indicate that it is a zone of thrust faulting that dips to the
northeast ( Armbruster et al . , 1978 ; Pennington , 1979 ) . The slip - direction is
approximately perpendicular to the strike of the IKSZ . This is similar to
observations ...
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 344
and Arunachal in the east , similar fauna and flora is found . In the latter area
volcanic rocks ( Abor Traps ) of probably the same age as the Panial Traps ( Jain
et al . , 1974 ) are exposed . Obviously , while Cambrian to Carboniferous
sequence ...
and Arunachal in the east , similar fauna and flora is found . In the latter area
volcanic rocks ( Abor Traps ) of probably the same age as the Panial Traps ( Jain
et al . , 1974 ) are exposed . Obviously , while Cambrian to Carboniferous
sequence ...
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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