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 283
... active on the basis of the teleseismic data , but the density of faults , their sometimes shallow dips , and the limits of tele- seismic locations prohibit this in many cases . Data most useful in identifying active surface faults as active ...
... active on the basis of the teleseismic data , but the density of faults , their sometimes shallow dips , and the limits of tele- seismic locations prohibit this in many cases . Data most useful in identifying active surface faults as active ...
Page 294
... active faults shown in Figure 1 indicates that the mapped active faults fall into the following four main types . 1. Transform faults . These faults comprise the western boundary of the Indo - Pakistan sub- continent indicating strong ...
... active faults shown in Figure 1 indicates that the mapped active faults fall into the following four main types . 1. Transform faults . These faults comprise the western boundary of the Indo - Pakistan sub- continent indicating strong ...
Page 352
... active trace of the Chaman fault , a narrow , linear feature on aerial photos , especially where it tra- verses late ... active trace , fault zone , and fault system based on field observations . The Active Trace In the Chaman segment ...
... active trace of the Chaman fault , a narrow , linear feature on aerial photos , especially where it tra- verses late ... active trace , fault zone , and fault system based on field observations . The Active Trace In the Chaman segment ...
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