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Page 1
Still less are known about the regularities of istribution of the endogenous
mineral deposits in this region , which are represented by a sufficiently broad
spectrum of re showings . Problems of metallogeny of West Pakistan have not
been ...
Still less are known about the regularities of istribution of the endogenous
mineral deposits in this region , which are represented by a sufficiently broad
spectrum of re showings . Problems of metallogeny of West Pakistan have not
been ...
Page 5
No less characteristic is the copper mineralization which is followed in some
cases by the molybdenum one . The youngest endogenous mineral formations
within the Chagai median massif are the sulphur deposits ; they are confined to
vents ...
No less characteristic is the copper mineralization which is followed in some
cases by the molybdenum one . The youngest endogenous mineral formations
within the Chagai median massif are the sulphur deposits ; they are confined to
vents ...
Page 9
On the scheme attached ( Fig . 2 ) are clearly shown the disposition of ore belts ;
the features of belt distribution of endogenous deposits within the southern part of
West Pakistan in relation to their age and type . Most conspicuously it is shown ...
On the scheme attached ( Fig . 2 ) are clearly shown the disposition of ore belts ;
the features of belt distribution of endogenous deposits within the southern part of
West Pakistan in relation to their age and type . Most conspicuously it is shown ...
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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