Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 6
... possible in Pliocene ) . Late ( the closing of the geosynclinal regime , transition to platformic one . Consolidation of folded structures , increasing role of rupture dislocations . Magmatism Chagai Median massif Native sulphur ...
... possible in Pliocene ) . Late ( the closing of the geosynclinal regime , transition to platformic one . Consolidation of folded structures , increasing role of rupture dislocations . Magmatism Chagai Median massif Native sulphur ...
Page 8
... possible . Besides , in some ore belts one or another type of prospective mineralization , which at present is not dominating there , is represented only by small ore manifestations though potential possibilities of the given minerali ...
... possible . Besides , in some ore belts one or another type of prospective mineralization , which at present is not dominating there , is represented only by small ore manifestations though potential possibilities of the given minerali ...
Page 12
... Possible extension of Hindubagh chromite zone ( II ) ; 25 - Zone of development of manganese , barite and barite - polymetallic deposits , chro mite being of minor significance ( within the zone , manifestation of iron ore and copper ...
... Possible extension of Hindubagh chromite zone ( II ) ; 25 - Zone of development of manganese , barite and barite - polymetallic deposits , chro mite being of minor significance ( within the zone , manifestation of iron ore and copper ...
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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