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Page 1
... direction from the Straits of Gibralter in the West to Malacca Peninsula in the
East Young , folded structures of the Tethys usually form distinctly lineated folded
belts clearly outlining numerous median massifs and projections of platforms .
... direction from the Straits of Gibralter in the West to Malacca Peninsula in the
East Young , folded structures of the Tethys usually form distinctly lineated folded
belts clearly outlining numerous median massifs and projections of platforms .
Page 2
... from the adjacent ones by a clearly expressed magmatization . Within the
Chagai median massif terrestrial effusives are of considerable development
whereas for the zone of central geosynclinal trough submarine volcanic rocks are
typical .
... from the adjacent ones by a clearly expressed magmatization . Within the
Chagai median massif terrestrial effusives are of considerable development
whereas for the zone of central geosynclinal trough submarine volcanic rocks are
typical .
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