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Page 5
The walls of the fracture are covered with crystals of columnar celestite , forming
symmetrical zones which are replaced to the centre of the cavity by zones of
sintered banded carbonate , bearing traces of origin from descending solutions .
The walls of the fracture are covered with crystals of columnar celestite , forming
symmetrical zones which are replaced to the centre of the cavity by zones of
sintered banded carbonate , bearing traces of origin from descending solutions .
Page 8
... within the belt should attract our greatest attention as in case of the presence of
direct ore indications ( the presence of fractures , disseminated mineralization )
which may be very favourable for the origin of major metasomatic ore deposits .
... within the belt should attract our greatest attention as in case of the presence of
direct ore indications ( the presence of fractures , disseminated mineralization )
which may be very favourable for the origin of major metasomatic ore deposits .
Page 9
... their origin with the period of principal folding phase in the central geosynclinal
trough . The upper age limit of mineralization is not fixed but probably it can be of
the Oligocene age as , since that t'me , signs of active intrusive activity on the ...
... their origin with the period of principal folding phase in the central geosynclinal
trough . The upper age limit of mineralization is not fixed but probably it can be of
the Oligocene age as , since that t'me , signs of active intrusive activity on the ...
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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