Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 2
... characteristic and this zone differs from the adjacent ones by a clearly expressed magmatization . Within the Chagai median massif terrestrial effusives are of considerable development whereas for the zone of central geosynclinal trough ...
... characteristic and this zone differs from the adjacent ones by a clearly expressed magmatization . Within the Chagai median massif terrestrial effusives are of considerable development whereas for the zone of central geosynclinal trough ...
Page 9
... characteristic that these deposits originate in the periphery of the geosyncline , in its northern marginal part , within the rigid structures of the Chagai median massif that are a consolidated enclosing rock of Alpine geosynclinal ...
... characteristic that these deposits originate in the periphery of the geosyncline , in its northern marginal part , within the rigid structures of the Chagai median massif that are a consolidated enclosing rock of Alpine geosynclinal ...
Page 10
... characteristic and endogenous mineral concentrations related with felsic and ultrafelsic granites are not typical . 7. As to the character of magmatism and endogenous metallogeny , the concerned region chiefly embracing the Baluchistan ...
... characteristic and endogenous mineral concentrations related with felsic and ultrafelsic granites are not typical . 7. As to the character of magmatism and endogenous metallogeny , the concerned region chiefly embracing the Baluchistan ...
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Common terms and phrases
Afghanistan Alpine geosynclinal antimony Baluchistan Alpine Baluchistan geosynclinal development barite barite-polymetallic Bela region border central geosynclinal trough central geosynclinal zone Chagai median massif chalcopyrite characteristic characterized chromite deposits chromite ore belt complex confined copper and molybdenum copper-molybdenum Cretaceous Dalbandin distribution of endogenous Early Paleogene endogenous deposits endogenous mineralization Eocene epithermal felsic Fluorite deposits folded structures formation formed fracture zones fractured intrusions gabbro geological development geological structure Geological Survey geosynclinal regime geosynclinal trough zone granodiorite hematite Hindubagh region hydrothermal Indian Platform Khuzdar Las Bela lenses limestones Magmatism magnetite main folding Makran manganese manifestations Mesozoic metallogenic features metallogeny mineral deposits molybdenum Neogene North Waziristan occur Oligocene orebearing structures Paleogene Pishin Pishin-Makran trough Pishin-Makran zone plagiogranites porphyrites Quetta regularities of distribution schists sedimentation skarn southern structural zones submarine effusives Survey of Pakistan terrestrial effusives Tethys thickness took place ultramafic intrusions ultramafic rocks volcanogenous West Pakistan widely developed