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 173
... occur both north and south of the suture zone but are mainly in low - grade ( com- monly greenschist facies ) metamorphic rocks or in rocks exhibiting little sign at all of metamor- phism . The host rocks are mainly clastics or car ...
... occur both north and south of the suture zone but are mainly in low - grade ( com- monly greenschist facies ) metamorphic rocks or in rocks exhibiting little sign at all of metamor- phism . The host rocks are mainly clastics or car ...
Page 181
... occur in a zone with strongly deformed sediments dipping below the Chagai volcanic arc , suggesting a subduction complex in the Ras Koh mountain range . The ophiolites in northern Pakistan occur in suture zones between the Eurasian ...
... occur in a zone with strongly deformed sediments dipping below the Chagai volcanic arc , suggesting a subduction complex in the Ras Koh mountain range . The ophiolites in northern Pakistan occur in suture zones between the Eurasian ...
Page 202
... occur within the schists near the amphibolite bands . After an intercalation of a pinkish granosyenite to granite gneiss , with large pinkish " square " orthoclases , come garnet schists and amphibolites grading into hornblendites ...
... occur within the schists near the amphibolite bands . After an intercalation of a pinkish granosyenite to granite gneiss , with large pinkish " square " orthoclases , come garnet schists and amphibolites grading into hornblendites ...
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
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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