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Page 1
Probably was Tvalchrelidze ( 1964 ) who first briefly characterized the most
specific metallogenous features of the Baluchistan meillogenous province ,
emphasizing special significance of chromite mineralization for the Western
fringe of the ...
Probably was Tvalchrelidze ( 1964 ) who first briefly characterized the most
specific metallogenous features of the Baluchistan meillogenous province ,
emphasizing special significance of chromite mineralization for the Western
fringe of the ...
Page 2
In general the Baluchistan geosyncline is characterized by a weak manifestation
of intrusive magmatism and rather subordinate significance of granitoidal rocks
with extremely constrasting display of derivative ultramafic and mafic magmas .
In general the Baluchistan geosyncline is characterized by a weak manifestation
of intrusive magmatism and rather subordinate significance of granitoidal rocks
with extremely constrasting display of derivative ultramafic and mafic magmas .
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