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
... 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 It is a north ...
... 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 It is a north ...
Page 288
... located to the west of Zhob and north of Qila Saifullah . These faults run , parallel to the general strike , through Late Tertiary rock for- mations . One of these faults ( 13 a ) , located along the eastern margin of Shinghar range ...
... located to the west of Zhob and north of Qila Saifullah . These faults run , parallel to the general strike , through Late Tertiary rock for- mations . One of these faults ( 13 a ) , located along the eastern margin of Shinghar range ...
Page 289
... located along these fractures , mainly near the northern end of the fracture zone . 32. The Peshawar Basin fault zone - The pecu- liar drainage pattern of the Peshawar Basin , series of stream offsets , traces of lineaments that may be ...
... located along these fractures , mainly near the northern end of the fracture zone . 32. The Peshawar Basin fault zone - The pecu- liar drainage pattern of the Peshawar Basin , series of stream offsets , traces of lineaments that may be ...
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