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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
In the central geosynclinal trough zone at the early stage of geosynclinal
development , the formation of manganese , barite - polymetallic and chromite
deposits took place . The formation of pyrite type deposits is believed to occur at
this stage ...
In the central geosynclinal trough zone at the early stage of geosynclinal
development , the formation of manganese , barite - polymetallic and chromite
deposits took place . The formation of pyrite type deposits is believed to occur at
this stage ...
Page 10
First of all it concerns lead , which concentrates both in barite ores of early stage
and forms independent ore manifestations in the middle stage . One can suppose
that barite and mercury mineralizations can be displayed both in early and later ...
First of all it concerns lead , which concentrates both in barite ores of early stage
and forms independent ore manifestations in the middle stage . One can suppose
that barite and mercury mineralizations can be displayed both in early and later ...
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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