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 70
... Gondwanaland , ( see Table 5 ) , and associated circles of confidence ( 95 , level ) , pootted against the Smith and ... Gondwanaland on the Smith and Hallam reconstruction ( A ) . Table 5A . Mean palaeomagnetic south poles for western ...
... Gondwanaland , ( see Table 5 ) , and associated circles of confidence ( 95 , level ) , pootted against the Smith and ... Gondwanaland on the Smith and Hallam reconstruction ( A ) . Table 5A . Mean palaeomagnetic south poles for western ...
Page 75
... Gondwanaland , it has been concluded that during the Permian . eastern Gondwanaland lagged behind western Gondwanaland in the course of a large counter- clockwise rotational movement , with a possible partly catching up during the ...
... Gondwanaland , it has been concluded that during the Permian . eastern Gondwanaland lagged behind western Gondwanaland in the course of a large counter- clockwise rotational movement , with a possible partly catching up during the ...
Page 105
... Gondwanaland did not occur until after Early Cretaceous time . Recently , Smith and Briden ( 1977 ) produced computer - drawn Mesozoic and Cenozoic ... Gondwanaland concept relate to the Gondwanaland and the Pakistan Region 105.
... Gondwanaland did not occur until after Early Cretaceous time . Recently , Smith and Briden ( 1977 ) produced computer - drawn Mesozoic and Cenozoic ... Gondwanaland concept relate to the Gondwanaland and the Pakistan Region 105.
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