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 41
... Tertiary are still very scant , but the late Palaeozoic to early Tertiary section of the Indo - Pakistani APW seems reasonably well established . For the remainder of the Tertiary only DSDP core results are available and these add only ...
... Tertiary are still very scant , but the late Palaeozoic to early Tertiary section of the Indo - Pakistani APW seems reasonably well established . For the remainder of the Tertiary only DSDP core results are available and these add only ...
Page 56
... Tertiary ( McKenzie and Sclater , 1971 ; Powell , this volume ) . Although determination of the duration of polarity epochs , especially during the late Cretaceous and the early Tertiary is still open to refinement ( Heirtzler et al ...
... Tertiary ( McKenzie and Sclater , 1971 ; Powell , this volume ) . Although determination of the duration of polarity epochs , especially during the late Cretaceous and the early Tertiary is still open to refinement ( Heirtzler et al ...
Page 66
... Tertiary reconstruction of the Gondwanaland continents and Asia . The suggested position of Asia is according to the mean early Tertiary data for Europe , because of the paucity of early Tertiary palaeomagnetic data for Asia . African ...
... Tertiary reconstruction of the Gondwanaland continents and Asia . The suggested position of Asia is according to the mean early Tertiary data for Europe , because of the paucity of early Tertiary palaeomagnetic data for Asia . African ...
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