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 175
... deposits . In at least some cases , contact with carbonate rocks appears to have created suitable deposi- tional ... deposits . Even if parts of the Karakorum batholith prove to be subduction - related , they appear to be poorly ...
... deposits . In at least some cases , contact with carbonate rocks appears to have created suitable deposi- tional ... deposits . Even if parts of the Karakorum batholith prove to be subduction - related , they appear to be poorly ...
Page 177
... deposits in the Darjeeling region of West Bengal and Sikkim . Ores consist of iron , copper , lead and zinc sulphides and minor sulphosalts exhibiting compositional lamination and large - scale conformity with the Daling Series host ...
... deposits in the Darjeeling region of West Bengal and Sikkim . Ores consist of iron , copper , lead and zinc sulphides and minor sulphosalts exhibiting compositional lamination and large - scale conformity with the Daling Series host ...
Page 328
... deposit is similar to many of the more recent alluvial fan deposits , except in the relative abundance of rounded pebbles of Kamerod type . The precise age of this deposit is unknown ; it is possibly of Late Pliocene rather than ...
... deposit is similar to many of the more recent alluvial fan deposits , except in the relative abundance of rounded pebbles of Kamerod type . The precise age of this deposit is unknown ; it is possibly of Late Pliocene rather than ...
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