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Page 2
The latter are widely 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 ...
The latter are widely 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 ...
Page 5
The youngest endogenous mineral formations within the Chagai median massif
are the sulphur deposits ; they are confined to vents of Early Quarternary
volcanoes . To the north of Koh - Kundi they form complicated and major volcanic
...
The youngest endogenous mineral formations within the Chagai median massif
are the sulphur deposits ; they are confined to vents of Early Quarternary
volcanoes . To the north of Koh - Kundi they form complicated and major volcanic
...
Page 9
The third , copper - molybdenum ore belt is confined to the Chagai median massif
within which as mentioned above , fracture intrusions of intermediate to alkaline
rocks followed by copper and molybdenum mineralization has a great ...
The third , copper - molybdenum ore belt is confined to the Chagai median massif
within which as mentioned above , fracture intrusions of intermediate to alkaline
rocks followed by copper and molybdenum mineralization has a great ...
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Common terms and phrases
analysis antimony associated Baluchistan geosyncline barite bearing Bela region belt bodies border central geosynclinal trough Chagai median massif characteristic characterized chromite deposits clearly closely complex composed confined connected consider consideration copper copper-molybdenum Cretaceous definite direction dislocations distinguishing Early effusives endogenous deposits endogenous mineralization epithermal evidently extends felsic fluorite fluorite deposits folded folded structures formation formed fracture zones fractured geological geosynclinal development Hindubagh Indian Platform iron known largest late lenses limestones limits Magmatism magnetite major manganese manifestations marginal marked meridional metallogeny mineral deposits molybdenum Neogene northern observe occur Oligocene origin outlined Paleogene period Pishin position possible present processes prominent region regularities of distribution relation represented rocks Scheme sedimentation sequences significance situated skarn southern stage structural zones structures studied tectonic terrestrial territory Tethys thickness took traced ultramafic intrusions ultramafic rocks veins volcanic volcanogenous West Pakistan widely developed zone