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Page 5
A particulr position is occupied by the celestite deposits situated to the west of
Hyderabad . The deposit seems to be of infiltration type . The most prominent of
them is shown by an open fracture from 0.15 m to 0.5 m in width cutting
horizontally ...
A particulr position is occupied by the celestite deposits situated to the west of
Hyderabad . The deposit seems to be of infiltration type . The most prominent of
them is shown by an open fracture from 0.15 m to 0.5 m in width cutting
horizontally ...
Page 8
One can distinguish here three ore belts , their borders coinciding with the
position of the main structural zones : ( a ) chromite ore belt confined to the axial
part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the ...
One can distinguish here three ore belts , their borders coinciding with the
position of the main structural zones : ( a ) chromite ore belt confined to the axial
part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the ...
Page 9
These belts are formed in the place of tectonic zones which are characterized by
a different type of development and their position in space is defined at present
by the position of their strụctural borders . On the scheme attached ( Fig .
These belts are formed in the place of tectonic zones which are characterized by
a different type of development and their position in space is defined at present
by the position of their strụctural borders . On the scheme attached ( Fig .
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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