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 204
... granite crop out . The granites increase in fre- quency upstream , intruding into vertical , to steep- ly south - dipping , amphibolites and hornblende gneisses , the latter containing impressive aplitic and pegmatitic dike swarms ...
... granite crop out . The granites increase in fre- quency upstream , intruding into vertical , to steep- ly south - dipping , amphibolites and hornblende gneisses , the latter containing impressive aplitic and pegmatitic dike swarms ...
Page 205
... granite , somewhat similar to young tourmaline granites ( Malakand granite ) ; contains large xenoliths of Dogra - type slates . 3 ) Thick bedded marbles , probably on top of granite . 4 ) Muscovite granite gneiss , similar to Mindora ...
... granite , somewhat similar to young tourmaline granites ( Malakand granite ) ; contains large xenoliths of Dogra - type slates . 3 ) Thick bedded marbles , probably on top of granite . 4 ) Muscovite granite gneiss , similar to Mindora ...
Page 206
... granite gneiss layers . D = Dir ; LP = Lowari Pass , 3050 m ; M = Mirkhani ; CH = Chitral River . the northeast strike of Chitral . This structural trend is cut by younger granites which , based on the cursory observations , show little ...
... granite gneiss layers . D = Dir ; LP = Lowari Pass , 3050 m ; M = Mirkhani ; CH = Chitral River . the northeast strike of Chitral . This structural trend is cut by younger granites which , based on the cursory observations , show little ...
Contents
Tectonic evolution of the Tien Shan Pamir and Karakorum | 25 |
A review of palaeomagnetic data from the IndoPakistan fragment | 41 |
PalaeozoicMesozoic biostratigraphy of Pakistan in relation | 81 |
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active Afghanistan anomalies Asia Baluchistan basin beds Bela Bibai blocks boundary Carboniferous Cenozoic Chaman fault Chitral chromite 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 massif melange Mesozoic metamorphic mineralization Molnar mountain belt Muslim Bagh northern northward occur oceanic ophiolite belt ophiolites orogenic palaeomagnetic palaeomagnetic data Palaeozoic Paleocene Pamir Permian plate polarity pole Quetta region Ridge rocks Salt Range sandstones schists sedimentary sediments seismicity 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