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. |
From inside the book
Results 1-3 of 45
Page 209
... belts within the ophiolite zone in contrast to the rapid changes in east - west sections . Steep melange zones tectonically cut the pillow lava belt . Fre- quently , gabbros are related to these zones . Of special interest are melange ...
... belts within the ophiolite zone in contrast to the rapid changes in east - west sections . Steep melange zones tectonically cut the pillow lava belt . Fre- quently , gabbros are related to these zones . Of special interest are melange ...
Page 267
... ophiolite belt of those rock types which are not proper ophiolites ( i.e. , the ultramafics , gabbro , and the pillow lavas without sediments - cf . Cole- man , 1977 , p . 6-7 ) , but rock types such as pelagic sediments with gabbros or ...
... ophiolite belt of those rock types which are not proper ophiolites ( i.e. , the ultramafics , gabbro , and the pillow lavas without sediments - cf . Cole- man , 1977 , p . 6-7 ) , but rock types such as pelagic sediments with gabbros or ...
Page 268
... belt of the axial ophiolite belt " , Stöcklin , 1977 ) . The melanges in the sub- belt and the Bela belt also appear similar . The main difference between the ophiolites of the Iranian sub - belt and those of the Bela belt is the ...
... belt of the axial ophiolite belt " , Stöcklin , 1977 ) . The melanges in the sub- belt and the Bela belt also appear similar . The main difference between the ophiolites of the Iranian sub - belt and those of the Bela belt is the ...
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
Copyright | |
18 other sections not shown
Other editions - View all
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