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 155
... ( Figure 10 ) . Rocks from the Rohtas structure were studied as early as 1913 by Pilgrim , and later by De Terra and De Chardin ( 1936 ) and Kravchenko ( 1965 ) . Those workers concluded that much of the struc- ture was composed of rocks ...
... ( Figure 10 ) . Rocks from the Rohtas structure were studied as early as 1913 by Pilgrim , and later by De Terra and De Chardin ( 1936 ) and Kravchenko ( 1965 ) . Those workers concluded that much of the struc- ture was composed of rocks ...
Page 311
... Figure 7. Lower hemisphere projections of the focal mechanisms of events A and B ( Figure 8 ) are shown with dark shading of the quadrants of compressional arrivals . The tensional axis is indicated ( T ) . The line XX indicates the ...
... Figure 7. Lower hemisphere projections of the focal mechanisms of events A and B ( Figure 8 ) are shown with dark shading of the quadrants of compressional arrivals . The tensional axis is indicated ( T ) . The line XX indicates the ...
Page 352
... Figure 2 O Quetta Nushki Figure 4 오 Karachi 50 KM Figure 1. Regional relations of Chaman fault in Pakistan . Eurasian plates which includes the Chaman , Ornach Nal , and other faults . In this subdivision the Chaman fault features are ...
... Figure 2 O Quetta Nushki Figure 4 오 Karachi 50 KM Figure 1. Regional relations of Chaman fault in Pakistan . Eurasian plates which includes the Chaman , Ornach Nal , and other faults . In this subdivision the Chaman fault features are ...
Contents
Tectonic evolution of the Tien Shan Pamir and Karakorum | 25 |
A review of palaeomagnetic data from the IndoPakistan fragment | 41 |
PalaeozoicMesozoic biostratigraphy of Pakistan in relation | 81 |
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active Afghanistan anomalies Asia Baluchistan basin beds Bela Bibai blocks boundary Carboniferous Cenozoic Chaman fault Chitral chromite 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 massif melange Mesozoic metamorphic mineralization Molnar mountain belt Muslim Bagh northern northward occur oceanic ophiolite belt ophiolites orogenic palaeomagnetic palaeomagnetic data Palaeozoic Paleocene Pamir Permian plate polarity pole Quetta region Ridge rocks Salt Range sandstones schists sedimentary sediments seismicity 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