Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 3
... confined to the central trough of the Baluchistan geosyncline within which geosynclinal carbonate complexes and submarine effusives are widely developed . There is a distinct relation between the massifs of ultramafic rocks with arge ...
... confined to the central trough of the Baluchistan geosyncline within which geosynclinal carbonate complexes and submarine effusives are widely developed . There is a distinct relation between the massifs of ultramafic rocks with arge ...
Page 8
... confined to the axial part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the territory of the late Pishin - Makran geosynclinal trough and ( c ) copper - molybdenum belt confined to the Chagai median massif ...
... confined to the axial part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the territory of the late Pishin - Makran geosynclinal trough and ( c ) copper - molybdenum belt confined to the Chagai median massif ...
Page 12
... confined to the central part of the geosynclinal trough ; 2 - Copper - Molybdenum ore belt ( II ) confined to Chagai median massif and formed in the middle stages of the geosynclinal development on the borderline of the Eocene and ...
... confined to the central part of the geosynclinal trough ; 2 - Copper - Molybdenum ore belt ( II ) confined to Chagai median massif and formed in the middle stages of the geosynclinal development on the borderline of the Eocene and ...
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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