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 9
... basin and its coun- terpart off the SW margin of India , formed during this period . How far back the distant pole of rotation should be continued is not certain , since beyond Ma 28 the fracture zones in the Madagascar basin become ...
... basin and its coun- terpart off the SW margin of India , formed during this period . How far back the distant pole of rotation should be continued is not certain , since beyond Ma 28 the fracture zones in the Madagascar basin become ...
Page 31
... basin , the Petr- Transalai " saddle " , the Alai trough , the Transalai zone and the Kashgar Basin . During the Early Carboniferous , when Eugeo- synclines and oceanic crust were generated in South Ghissar and Northern Pamir , the ...
... basin , the Petr- Transalai " saddle " , the Alai trough , the Transalai zone and the Kashgar Basin . During the Early Carboniferous , when Eugeo- synclines and oceanic crust were generated in South Ghissar and Northern Pamir , the ...
Page 289
... Basin fault zone - The pecu- liar drainage pattern of the Peshawar Basin , series of stream offsets , traces of lineaments that may be seen of Landsat imagery , and the fact that this basin is located at a point where there are sharp ...
... Basin fault zone - The pecu- liar drainage pattern of the Peshawar Basin , series of stream offsets , traces of lineaments that may be seen of Landsat imagery , and the fact that this basin is located at a point where there are sharp ...
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