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 98
... blocks with provincially exotic faunas . Were these perhaps derived from the sedi- mentary wedge that formerly extended along the Tibetan margin prior to the intercontinental collision between the Indo - Pak and Asian blocks ? Are they ...
... blocks with provincially exotic faunas . Were these perhaps derived from the sedi- mentary wedge that formerly extended along the Tibetan margin prior to the intercontinental collision between the Indo - Pak and Asian blocks ? Are they ...
Page 344
... Blocks . Thick arrows show the direction of movements of different blocks relative to one another along fault zones marked 1 , 2 , 3 , and 4 . ( b - d ) Scheme of the tectonic relations of the Indo- Pakistan block and surrounding blocks ...
... Blocks . Thick arrows show the direction of movements of different blocks relative to one another along fault zones marked 1 , 2 , 3 , and 4 . ( b - d ) Scheme of the tectonic relations of the Indo- Pakistan block and surrounding blocks ...
Page 355
... blocks of vein quartz Fine grained metamorphic Quartz ' diorite A Serpentinite ' Block of Figure 5. Chaman fault ... blocks of the ultramafic rock are found in the Chaman fault zone only north of this branch fault . South of the Chaman ...
... blocks of vein quartz Fine grained metamorphic Quartz ' diorite A Serpentinite ' Block of Figure 5. Chaman fault ... blocks of the ultramafic rock are found in the Chaman fault zone only north of this branch fault . South of the Chaman ...
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