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 25
... Tien Shan , Pamir and Karakorum the southward migration of the mobile belts reflects the growth of the Eurasian continent during the Phanerozoic . Geosynclinal develop- ment in the mobile belts began with rifting and drifting of Pre ...
... Tien Shan , Pamir and Karakorum the southward migration of the mobile belts reflects the growth of the Eurasian continent during the Phanerozoic . Geosynclinal develop- ment in the mobile belts began with rifting and drifting of Pre ...
Page 29
... Tien Shan eugeosyncline may have been formed upon oceanic crust which is still partially preserved as an ultrabasic - gabbroic ( ophiolitic ) rock sequence ( Makarychev , 1974 ) . The presence of ... Tien Shan , Pamir and Karakorum 29.
... Tien Shan eugeosyncline may have been formed upon oceanic crust which is still partially preserved as an ultrabasic - gabbroic ( ophiolitic ) rock sequence ( Makarychev , 1974 ) . The presence of ... Tien Shan , Pamir and Karakorum 29.
Page 37
... Tien Shan , Trans - Tien Shan , South- west Pamir - Nuristan All development occurs on top of cratonic crust , the final products being median massifs and basins . ( In the Middle Tien Shan , however , indications for rifting during the ...
... Tien Shan , Trans - Tien Shan , South- west Pamir - Nuristan All development occurs on top of cratonic crust , the final products being median massifs and basins . ( In the Middle Tien Shan , however , indications for rifting during the ...
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
Copyright | |
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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