Geodynamics of Pakistan"Geodynamics is dominated by plate tectonic models. Plate tectonics promises to provide explanation of global geodynamics including the origin of earthquakes, volcanoes and mountain building... This volume provide a comprehensive view of the geodynamic framework in which the evolution took place..." Preface. |
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Page 43
... Klootwijk , 1976 ) , is a questionable procedure in the light of such new data as that presented for the early Palaeozoic of Australia by Klootwijk ( 1978a , b , c ) . Backwards extension of the APW to about 750 m . y . to include the ...
... Klootwijk , 1976 ) , is a questionable procedure in the light of such new data as that presented for the early Palaeozoic of Australia by Klootwijk ( 1978a , b , c ) . Backwards extension of the APW to about 750 m . y . to include the ...
Page 47
... KLOOTWIJK ( 1974 ) A KLOOTWIJK ( 1976 ) PH25 PANJAL TRAPS M. Carboniferous- L. Triassic 74.8E 34.1N 30mT 580 ° C 12 ( 34 ) 156.5 +32.5 19.8 9.9 33.65 101.9E in 11.2 6.3 D MCELHINNY ET AL . ( press PH26 PACHMAPH : BEDS 78.8E 22.8N 280mT ...
... KLOOTWIJK ( 1974 ) A KLOOTWIJK ( 1976 ) PH25 PANJAL TRAPS M. Carboniferous- L. Triassic 74.8E 34.1N 30mT 580 ° C 12 ( 34 ) 156.5 +32.5 19.8 9.9 33.65 101.9E in 11.2 6.3 D MCELHINNY ET AL . ( press PH26 PACHMAPH : BEDS 78.8E 22.8N 280mT ...
Page 54
... ( Klootwijk 1974d ) . E. Upper Bhander Sandstones from the Great Vindhyan Basin ( Klootwijk 1973 ) . In this case , symbol = 1 denotes the direction of secondary magnetization components eliminated by thermal methods and alternating field ...
... ( Klootwijk 1974d ) . E. Upper Bhander Sandstones from the Great Vindhyan Basin ( Klootwijk 1973 ) . In this case , symbol = 1 denotes the direction of secondary magnetization components eliminated by thermal methods and alternating field ...
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
Copyright | |
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Common terms and phrases
active Afghanistan anomalies Baluchistan basin beds Bela Bibai blocks boundary Carboniferous Cenozoic Chaman fault Chitral chromite continental Cretaceous crust crustal Deccan Trap deformation deposits Desio dunite earthquake east eastern emplaced Eocene Eurasia Farah fault zone faunas Figure fold Formation gabbro Gansser GEODYNAMICS Geol Geological Survey Geophys gneisses Gondwanaland granite Greater India Hazara Himalaya Hindu IBID India Indo-Pakistan Indus Suture Iran Jour Jurassic Karakorum Klootwijk Late lavas limestones located lower magnetic Makran margin massif melange Mesozoic metamorphic mineralization Molnar mountain belt Muslim Bagh northern northward occur oceanic ophiolite belt ophiolites orogenic palaeomagnetic Palaeozoic Paleocene Pamir Permian plate polarity pole Quetta region Ridge rocks Salt Range sandstones schists sedimentary sediments seismic sequence serpentinite shales Siwalik southern stratigraphic structure subcontinent subduction Survey of Pakistan Syntaxis tectonic Tertiary thick thrust Tien Shan trending Triassic ultramafic Upper volcanic West Pakistan western Zhob Valley