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 35
... Central and Southeast Pamir Central and Southeast Pamir were deformed during the Alpine orogeny , with sedimentation in the Paleozoic , rifting in the Carboniferous- Middle Triassic , island arc formation in the Late Triassic - Jurassic ...
... Central and Southeast Pamir Central and Southeast Pamir were deformed during the Alpine orogeny , with sedimentation in the Paleozoic , rifting in the Carboniferous- Middle Triassic , island arc formation in the Late Triassic - Jurassic ...
Page 36
... Central Pamir several anticlinoria and synclinoria can be distinguished , with imbricated faults , major overthrusts , recumbent folds and overturned folds ( toward the north in the southern part of the mountain belt ) . The Central ...
... Central Pamir several anticlinoria and synclinoria can be distinguished , with imbricated faults , major overthrusts , recumbent folds and overturned folds ( toward the north in the southern part of the mountain belt ) . The Central ...
Page 320
... central Iran , one of which is Bazman . The large Iranian volcano of Taftan does not fall on either chain , but is located between the two chains in both a north - south and an east - west sense . The transverse breaks that separate the ...
... central Iran , one of which is Bazman . The large Iranian volcano of Taftan does not fall on either chain , but is located between the two chains in both a north - south and an east - west sense . The transverse breaks that separate the ...
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