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 287
... trending fault , located along the eastern margin of Bhalla Dhor valley near Kirdagap . It may be traced for about 20 miles . The fault trace cuts across the Recent alluvium and the Late Pleis- tocene gravels . -- 4. The Hudishi fault ...
... trending fault , located along the eastern margin of Bhalla Dhor valley near Kirdagap . It may be traced for about 20 miles . The fault trace cuts across the Recent alluvium and the Late Pleis- tocene gravels . -- 4. The Hudishi fault ...
Page 288
... trending fault near Kingri village . The fault trace intersects the Barkan fault , and near this inter- section a very large number of earthquake epi- centres are located . The Kingri fault is apparent- ly a left lateral wrench fault ...
... trending fault near Kingri village . The fault trace intersects the Barkan fault , and near this inter- section a very large number of earthquake epi- centres are located . The Kingri fault is apparent- ly a left lateral wrench fault ...
Page 289
... trending faults , some of which may have been active in Recent times . A number of earthquake epicentres are located in this Basin , some of which fall on the fault traces . - 33. The Nowshera ( a ) and Kund ( b ) faults There are two ...
... trending faults , some of which may have been active in Recent times . A number of earthquake epicentres are located in this Basin , some of which fall on the fault traces . - 33. The Nowshera ( a ) and Kund ( b ) faults There are two ...
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