Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 2
... geosynclinal trough 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 ...
... geosynclinal trough 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 ...
Page 9
... Baluchistan geosynclinal development with the evolution of which , the origin of magmatic , skarn and hydrothermal deposits of various mineral resources is connected . Typomorphic elements for the given region are : chrome , barite ...
... Baluchistan geosynclinal development with the evolution of which , the origin of magmatic , skarn and hydrothermal deposits of various mineral resources is connected . Typomorphic elements for the given region are : chrome , barite ...
Page 10
closely connected with the Baluchistan geosynclinal development , it is in fact beyond its limits as if going away laterally and locating itself among rigid structures of geosynclinal enclosing rock . The formation of the supposed ...
closely connected with the Baluchistan geosynclinal development , it is in fact beyond its limits as if going away laterally and locating itself among rigid structures of geosynclinal enclosing rock . The formation of the supposed ...
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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