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 173
... mineralization can be only in- directly determined , but mineralized structures at Krinj , Kaldam Gol and Awireth Gol cut for- mations as young as Cretaceous , at Faqir Moham- med of probable Eocene age , and at Ushu prob- able ...
... mineralization can be only in- directly determined , but mineralized structures at Krinj , Kaldam Gol and Awireth Gol cut for- mations as young as Cretaceous , at Faqir Moham- med of probable Eocene age , and at Ushu prob- able ...
Page 176
... Mineralization possibly related to Anatectic Granites As in the northwest Himalaya , there is appar- ently little significant metallic mineralization obviously associated with granitic rocks , either in the Lower Himalaya or in the ...
... Mineralization possibly related to Anatectic Granites As in the northwest Himalaya , there is appar- ently little significant metallic mineralization obviously associated with granitic rocks , either in the Lower Himalaya or in the ...
Page 177
... mineralization in Precamb- rian and Palaeozoic high- and low - grade meta- morphic rocks has been assigned to this category by Das Gupta et al . ( 1976 ) , the majority of it being considered to have possessed an originally syngenetic ...
... mineralization in Precamb- rian and Palaeozoic high- and low - grade meta- morphic rocks has been assigned to this category by Das Gupta et al . ( 1976 ) , the majority of it being considered to have possessed an originally syngenetic ...
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