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Page 2
The most eastern regions of the discussed territory belong to the Indian Platform ,
the structures of which are overlain by thick recent ... Unfortunately , up - till now
many cardinal points of the geological development of the region remain vague .
The most eastern regions of the discussed territory belong to the Indian Platform ,
the structures of which are overlain by thick recent ... Unfortunately , up - till now
many cardinal points of the geological development of the region remain vague .
Page 3
The upper age limit of the ultramafic intrusions of the Hindubagh region is of the
Eocene age . This conclusion is due to the fact that limestones containing fauna
of this age obviously supersimpose the weathered surface of the ultramafic rocks
.
The upper age limit of the ultramafic intrusions of the Hindubagh region is of the
Eocene age . This conclusion is due to the fact that limestones containing fauna
of this age obviously supersimpose the weathered surface of the ultramafic rocks
.
Page 8
Distinguishing such regional ore bearing structures has been done , to a great
extent provisionally , which is first of all due to ... belt whereas in the southern part
of the Las Bela region barite and barite - galena mineralization is most important .
Distinguishing such regional ore bearing structures has been done , to a great
extent provisionally , which is first of all due to ... belt whereas in the southern part
of the Las Bela region barite and barite - galena mineralization is most important .
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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