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 60
... Palaeozoic ( 8A ) and from the early Palaeozoic to the Triassic Jurassic ( 8B ) , plotted according to the Smith and Hallam reconstruction . The northern boundary of the Indo - Pakistan subcontinent is not well defined ; " Greater ...
... Palaeozoic ( 8A ) and from the early Palaeozoic to the Triassic Jurassic ( 8B ) , plotted according to the Smith and Hallam reconstruction . The northern boundary of the Indo - Pakistan subcontinent is not well defined ; " Greater ...
Page 81
... Palaeozoic - Mesozoic biostratigraphy of Pakistan , especially the northern mountainous region , is given providing , inter alia , preliminary reports of the presence of unequivocal Ordovician ( NE Chitral ) , Silurian ( Peshawar ...
... Palaeozoic - Mesozoic biostratigraphy of Pakistan , especially the northern mountainous region , is given providing , inter alia , preliminary reports of the presence of unequivocal Ordovician ( NE Chitral ) , Silurian ( Peshawar ...
Page 89
... Palaeozoic faunas ; our comments , accordingly , will be con- cerned primarily with zoogeographic relationships among Palaeozoic faunas and specifically the Devonian and Permian faunas that bulk so large in the new data presented here ...
... Palaeozoic faunas ; our comments , accordingly , will be con- cerned primarily with zoogeographic relationships among Palaeozoic faunas and specifically the Devonian and Permian faunas that bulk so large in the new data presented here ...
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