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Page 2
Here belong such important questions as the time of main folding , scope and
time of manifestation of basic stages of the ... One should evidently refer the initial
stage of the Baluchistan geosyncline to the late Paleozoic period when , in the ...
Here belong such important questions as the time of main folding , scope and
time of manifestation of basic stages of the ... One should evidently refer the initial
stage of the Baluchistan geosyncline to the late Paleozoic period when , in the ...
Page 9
In the central geosynclinal trough zone at the early stage of geosynclinal
development , the formation of manganese , barite - polymetallic and chromite
deposits took place . The formation of pyrite type deposits is believed to occur at
this stage ...
In the central geosynclinal trough zone at the early stage of geosynclinal
development , the formation of manganese , barite - polymetallic and chromite
deposits took place . The formation of pyrite type deposits is believed to occur at
this stage ...
Page 10
The formation of the supposed mercuryantimony belt is connected with the later
stage of development , the belt being the youngest and practically not
investigated at all . Thus in each stage of the Baluchistan geosynclinal
development , the ...
The formation of the supposed mercuryantimony belt is connected with the later
stage of development , the belt being the youngest and practically not
investigated at all . Thus in each stage of the Baluchistan geosynclinal
development , 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