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 219
... serpentinite reflect subaerial weathering conditions and diagenetic processes . These siliceous sediments pass into supratidal authigenic dolomites , which are twice interrupted by lateritic weathering deposits . The dolomites with ...
... serpentinite reflect subaerial weathering conditions and diagenetic processes . These siliceous sediments pass into supratidal authigenic dolomites , which are twice interrupted by lateritic weathering deposits . The dolomites with ...
Page 220
... serpentinite , in contrast to the Upper Cuisian - Lower Lutetian transgressions described above . The top part of the serpentinite includes blocks and deformed lenses of red Glo- botruncana - marls and micritic Maastrichtian lime ...
... serpentinite , in contrast to the Upper Cuisian - Lower Lutetian transgressions described above . The top part of the serpentinite includes blocks and deformed lenses of red Glo- botruncana - marls and micritic Maastrichtian lime ...
Page 245
... serpentinite is more than 1000 feet thick . Within the serpentinite " exotics " ( including radiolarite , marble , basalt , gabbro ) occur and become dominant south of the two massifs . The resulting melange , with serpenti- nite as ...
... serpentinite is more than 1000 feet thick . Within the serpentinite " exotics " ( including radiolarite , marble , basalt , gabbro ) occur and become dominant south of the two massifs . The resulting melange , with serpenti- nite as ...
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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Common terms and phrases
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