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Page 159
LISTRIC FAULTS AND THE HIMALAYAN EVOLUTION A.K.Dubey and M.I. Bhat
ABSTRACT Experimental structural studies on deformed physical models
suggest that the basement listric faults with curved strike have played a primary
control ...
LISTRIC FAULTS AND THE HIMALAYAN EVOLUTION A.K.Dubey and M.I. Bhat
ABSTRACT Experimental structural studies on deformed physical models
suggest that the basement listric faults with curved strike have played a primary
control ...
Page 173
However , the observation that cylindrical folds developed over the basement
faults suggested that the formation of arcuate folds , may probably require an
initial arcuation of the basement faults . Although we fail to visualize any definite ...
However , the observation that cylindrical folds developed over the basement
faults suggested that the formation of arcuate folds , may probably require an
initial arcuation of the basement faults . Although we fail to visualize any definite ...
Page 321
Green et al . , ( 1967 ) have also suggested that alkali basalts are derived by
fractionation at 35-60 km ; high ' al ' basalts at 15-35 km and ... This suggests that
Zhanskar basics were formed at greater depths as compared to Kumaun basics .
Green et al . , ( 1967 ) have also suggested that alkali basalts are derived by
fractionation at 35-60 km ; high ' al ' basalts at 15-35 km and ... This suggests that
Zhanskar basics were formed at greater depths as compared to Kumaun basics .
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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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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