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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... Quetta , Pakistan S. ANISUDDIN AHMAD Geological Survey of Pakistan Quetta , Pakistan FRANZ ALLEMANN Geologisches Institut Universitat Bern 3000 Bern , Switzerland JOHN ARMBRUSTER Lamont - Doherty Geological Observatory Columbia ...
... Quetta , Pakistan S. ANISUDDIN AHMAD Geological Survey of Pakistan Quetta , Pakistan FRANZ ALLEMANN Geologisches Institut Universitat Bern 3000 Bern , Switzerland JOHN ARMBRUSTER Lamont - Doherty Geological Observatory Columbia ...
Page 343
... Quetta Syntaxis usage The Quetta Syntaxis ( Wadia , 1953 ) is defined by a sharp southward swing , in the vicinity of Quetta , of the western ranges of the Sulaiman Arc ( Fig . 1 ) . The range trending southward from Quetta is the ...
... Quetta Syntaxis usage The Quetta Syntaxis ( Wadia , 1953 ) is defined by a sharp southward swing , in the vicinity of Quetta , of the western ranges of the Sulaiman Arc ( Fig . 1 ) . The range trending southward from Quetta is the ...
Page 346
... Quetta . The reasons for this obstruction at Quetta , which is directly responsible for the formation of the Quetta syntaxis , are not clear . Some suggestions , however , can be made . Assuming the basal decollement of the Sulai- man ...
... Quetta . The reasons for this obstruction at Quetta , which is directly responsible for the formation of the Quetta syntaxis , are not clear . Some suggestions , however , can be made . Assuming the basal decollement of the Sulai- man ...
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