Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 1
... developed within this zone , the total thickness of which reaches to 7 km . In the lower parts of the section of geosynclinal complexes , rocks of the Permian age are known ( which grades into the Triassic rocks ) . In the section of ...
... developed within this zone , the total thickness of which reaches to 7 km . In the lower parts of the section of geosynclinal complexes , rocks of the Permian age are known ( which grades into the Triassic rocks ) . In the section of ...
Page 2
... developed in the Chagai median massif and are practically absent in the zone of central ( axial ) geosynclinal trough where they are only represented by small massifs of plagiogranites . For the Pishin - Makran secondary trough zone ...
... developed in the Chagai median massif and are practically absent in the zone of central ( axial ) geosynclinal trough where they are only represented by small massifs of plagiogranites . For the Pishin - Makran secondary trough zone ...
Page 9
... developed within ore belt , it is represented by nonpros- pective genetic types which usually do not form important industrial quantities in similar structural conditions . On the contrary copper and molybdenum mineralizations in some ...
... developed within ore belt , it is represented by nonpros- pective genetic types which usually do not form important industrial quantities in similar structural conditions . On the contrary copper and molybdenum mineralizations in some ...
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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