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 215
... Eocene - lowermost Middle Eocene age ( Malguzar- , Muslim Bagh- and Jani River sections ) or of Lower Oligocene age ( Sor Dir section ) , Following the marine transgression , protected carbonate shelf facies prevails throughout Eocene ...
... Eocene - lowermost Middle Eocene age ( Malguzar- , Muslim Bagh- and Jani River sections ) or of Lower Oligocene age ( Sor Dir section ) , Following the marine transgression , protected carbonate shelf facies prevails throughout Eocene ...
Page 220
... Eocene to lowest Middle Eocene are found together with the white - colored planktonics of the G. lehneri zone , of Middle Eocene age ( All . 77302 , Fig . 13 ) . From 135-155m , thick hemipelagic authigenic marls alternate with about 60 ...
... Eocene to lowest Middle Eocene are found together with the white - colored planktonics of the G. lehneri zone , of Middle Eocene age ( All . 77302 , Fig . 13 ) . From 135-155m , thick hemipelagic authigenic marls alternate with about 60 ...
Page 233
... EOCENE ( LUTETIAN ) Upper MIDDLE EOCENE 160 150 77 305 - 77 304 - - 77308 - - 77307 77 303 140 130- -77 302 120 77 301 77306 110 77 300 100 с CORALGAL REEF coralliferous biopelsparite to pelmicrite , in parts coarse Lst - breccia ...
... EOCENE ( LUTETIAN ) Upper MIDDLE EOCENE 160 150 77 305 - 77 304 - - 77308 - - 77307 77 303 140 130- -77 302 120 77 301 77306 110 77 300 100 с CORALGAL REEF coralliferous biopelsparite to pelmicrite , in parts coarse Lst - breccia ...
Contents
K N Kravchenko | 25 |
Chris T Klootwijk | 41 |
John A Talent Ruth Mawson | 75 |
Copyright | |
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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