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Page 2
Within the Chagai median massif terrestrial effusives are of considerable
development whereas for the zone of central geosynclinal trough submarine
volcanic rocks are typical . In general the Baluchistan geosyncline is
characterized by a ...
Within the Chagai median massif terrestrial effusives are of considerable
development whereas for the zone of central geosynclinal trough submarine
volcanic rocks are typical . In general the Baluchistan geosyncline is
characterized by a ...
Page 7
Deposits Chromite , asbestos , magnesite Magnetite - epid deposits in (
hypergenous ) Barite , barite terrestrial effusives ; hematite polymetallic ; possibly
pyrite skarns along the contact of ores . limestones & felsic effusives . Magmatism
Early ...
Deposits Chromite , asbestos , magnesite Magnetite - epid deposits in (
hypergenous ) Barite , barite terrestrial effusives ; hematite polymetallic ; possibly
pyrite skarns along the contact of ores . limestones & felsic effusives . Magmatism
Early ...
Page 12
Legend I. - The Indian Platform ; 2- The Sargodha Schield ; 3 — The Central
geosynclinal through ; 4 — Areas of development of submarine effusives ; 5 —
The Chagai median massif ; 6 — Areas of development of terrestrial effusives ; 7
– Old ...
Legend I. - The Indian Platform ; 2- The Sargodha Schield ; 3 — The Central
geosynclinal through ; 4 — Areas of development of submarine effusives ; 5 —
The Chagai median massif ; 6 — Areas of development of terrestrial effusives ; 7
– Old ...
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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