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 149
... stratigraphic terminology of the Siwalik Group in Pakistan , and developed a tentative bio- stratigraphic scheme , based on the vertebrate fauna , for the Siwalik Group of the Potwar Plateau . Although the biostratigraphic approach of ...
... stratigraphic terminology of the Siwalik Group in Pakistan , and developed a tentative bio- stratigraphic scheme , based on the vertebrate fauna , for the Siwalik Group of the Potwar Plateau . Although the biostratigraphic approach of ...
Page 156
... stratigraphic sections , Figures 8 , 10 , 12 , 14 ) . The stratigraphic thickness enclosed by iso- chronous events , such as magnetic polarity reversals provides a direct measure of the net sedi- mentation rate . Figure 16 illustrates ...
... stratigraphic sections , Figures 8 , 10 , 12 , 14 ) . The stratigraphic thickness enclosed by iso- chronous events , such as magnetic polarity reversals provides a direct measure of the net sedi- mentation rate . Figure 16 illustrates ...
Page 159
... stratigraphic intervals possessing normal polarity . Refer to Figure 2 for magnetic reversal stratigraphic detail . Location of Basawa Kas section ( Figure 10 ) is illustrated . Polarity Stratigraphy 1000 950 450 900 440 850 800 750.
... stratigraphic intervals possessing normal polarity . Refer to Figure 2 for magnetic reversal stratigraphic detail . Location of Basawa Kas section ( Figure 10 ) is illustrated . Polarity Stratigraphy 1000 950 450 900 440 850 800 750.
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
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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