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Page 1
Problems of metallogeny of West Pakistan have not been discussed in geological
literature . Probably ... These investigations essentially xhaust all the works
where the analysis of metallogenic development of West Pakistan had been
given .
Problems of metallogeny of West Pakistan have not been discussed in geological
literature . Probably ... These investigations essentially xhaust all the works
where the analysis of metallogenic development of West Pakistan had been
given .
Page 9
MAIN CONCLUSIONS 1. Features of endogenous metallogeny of the southern
part of West Pakistan are principally defined by eugeosynclinal character of the
Baluchistan geosynclinal development with the evolution of which , the origin of ...
MAIN CONCLUSIONS 1. Features of endogenous metallogeny of the southern
part of West Pakistan are principally defined by eugeosynclinal character of the
Baluchistan geosynclinal development with the evolution of which , the origin of ...
Page 10
As to the character of magmatism and endogenous metallogeny , the concerned
region chiefly embracing the ... of de . posits are distinguished ; at the same time
each geosyncline has its own specific provincial metallogenic peculiarities .
As to the character of magmatism and endogenous metallogeny , the concerned
region chiefly embracing the ... of de . posits are distinguished ; at the same time
each geosyncline has its own specific provincial metallogenic peculiarities .
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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