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Page 2
One should evidently refer the initial stage of the Baluchistan geosyncline to the
late Paleozoic period when , in the marginal part of the Indian Platform a complex
system of meridional deep faults originated , breaking up the consolidated ...
One should evidently refer the initial stage of the Baluchistan geosyncline to the
late Paleozoic period when , in the marginal part of the Indian Platform a complex
system of meridional deep faults originated , breaking up the consolidated ...
Page 6
Platformic period Pleistocene ( the beginning is Deposits possible in Pliocene ) .
Native sulphur deposits in volcanic vents . Magmatism Old volcanoes :
agglomerates , tuffs and andesitic lavas . Oligocene and Miocene ( partly
Pliocene ? ) ...
Platformic period Pleistocene ( the beginning is Deposits possible in Pliocene ) .
Native sulphur deposits in volcanic vents . Magmatism Old volcanoes :
agglomerates , tuffs and andesitic lavas . Oligocene and Miocene ( partly
Pliocene ? ) ...
Page 9
In the middle stage of the Baluchistan geosynclinal development , referring in
time to the Early Neogene and corresponding to the period of main folding stages
, the formation of iron , copper and molybdenum deposits and ore manifestations
...
In the middle stage of the Baluchistan geosynclinal development , referring in
time to the Early Neogene and corresponding to the period of main folding stages
, the formation of iron , copper and molybdenum deposits and ore manifestations
...
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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