Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 2
... over- lain by thick recent deposits . Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline rocks forming the Sargodha Shield are known . It is worth mentioning that one of the features of the geological ...
... over- lain by thick recent deposits . Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline rocks forming the Sargodha Shield are known . It is worth mentioning that one of the features of the geological ...
Page 8
... overlain by the Oligocene deposits of late Pishin- Makran trough , due to which the belt is limited in width . Moreover it is not excluded , that within a single chromite ore belt , such as it is supposed to be at the present time ...
... overlain by the Oligocene deposits of late Pishin- Makran trough , due to which the belt is limited in width . Moreover it is not excluded , that within a single chromite ore belt , such as it is supposed to be at the present time ...
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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