Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 2
... submarine volcanic rocks are typical . In general the Baluchistan geosyncline is characterized by a weak manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely constrasting display ...
... submarine volcanic rocks are typical . In general the Baluchistan geosyncline is characterized by a weak manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely constrasting display ...
Page 3
... submarine effusives are widely developed . There is a distinct relation between the massifs of ultramafic rocks with arge zones of dislocations ; at the same time one can observe that the largest massifs are located in the regions of ...
... submarine effusives are widely developed . There is a distinct relation between the massifs of ultramafic rocks with arge zones of dislocations ; at the same time one can observe that the largest massifs are located in the regions of ...
Page 12
... submarine effusives ; 5 - The Chagai median massif ; 6 - Areas of development of terrestrial effusives ; 7 - Old Quarternary volcanoes ; 8 -- Late Pishin - Makran trough ; 9 - South Makran depression ; filled with Upper - Neogene ...
... submarine effusives ; 5 - The Chagai median massif ; 6 - Areas of development of terrestrial effusives ; 7 - Old Quarternary volcanoes ; 8 -- Late Pishin - Makran trough ; 9 - South Makran depression ; filled with Upper - Neogene ...
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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