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Page 2
For the Pishin - Makran secondary trough zone ; judging by recent data ,
magmatic formations are not characteristic and this zone differs from the adjacent
ones by a clearly expressed magmatization . Within the Chagai median massif ...
For the Pishin - Makran secondary trough zone ; judging by recent data ,
magmatic formations are not characteristic and this zone differs from the adjacent
ones by a clearly expressed magmatization . Within the Chagai median massif ...
Page 8
... belt confined to the axial part of the Baluchistan geosyncline , ( b ) mercury -
antimony belt occupying the territory of the late Pishin - Makran geosynclinal
trough and ( c ) copper - molybdenum belt confined to the Chagai median massif
( Fig .
... belt confined to the axial part of the Baluchistan geosyncline , ( b ) mercury -
antimony belt occupying the territory of the late Pishin - Makran geosynclinal
trough and ( c ) copper - molybdenum belt confined to the Chagai median massif
( Fig .
Page 12
... submarine effusives ; 5 — The Chagai median massif ; 6 — Areas of
development of terrestrial effusives ; 7 – Old Quarternary volcanoes ; 8 -- Late
Pishin - Makran trough ; 9 - South Makran depression ; filled with Upper -
Neogene molasses ...
... submarine effusives ; 5 — The Chagai median massif ; 6 — Areas of
development of terrestrial effusives ; 7 – Old Quarternary volcanoes ; 8 -- Late
Pishin - Makran trough ; 9 - South Makran depression ; filled with Upper -
Neogene molasses ...
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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