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. |
From inside the book
Results 1-3 of 88
Page 116
... formation spans the entire Permian . The Shaksgam Formation ( with flysch facies ) extends from the eastern Karakorum to western Tibet ; sections were described in the Shaksgam valley ( Desio , 1936 ) and the Shayok valley ( Dain- elli ...
... formation spans the entire Permian . The Shaksgam Formation ( with flysch facies ) extends from the eastern Karakorum to western Tibet ; sections were described in the Shaksgam valley ( Desio , 1936 ) and the Shayok valley ( Dain- elli ...
Page 333
... Formation and consists of the Cretaceous Bibai Formation and the Palaeocene Dungan Formation . Another thrust block , the Gogai nappe , with Middle Cretaceous rocks of the Parh Formation , overlies the Dungan Formation . The Bibai and ...
... Formation and consists of the Cretaceous Bibai Formation and the Palaeocene Dungan Formation . Another thrust block , the Gogai nappe , with Middle Cretaceous rocks of the Parh Formation , overlies the Dungan Formation . The Bibai and ...
Page 338
... Formation . In the autochtho- nous zone it overlies the Ghazij Formation . In the southern part of the allochthonous zone it over- lies the Dungan and the Parh Formations , and in the northern part of this zone it overlies the Wul- gai ...
... Formation . In the autochtho- nous zone it overlies the Ghazij Formation . In the southern part of the allochthonous zone it over- lies the Dungan and the Parh Formations , and in the northern part of this zone it overlies the Wul- gai ...
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
Copyright | |
18 other sections not shown
Other editions - View all
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