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Page 5
Fluorite and antimony deposits of epithermal type occurring in the central
geosynclinal zone and the late Pishin - Makran trough are formed in the Late
Paleogene and Neogene time . In any case the Pishin antimony deposits are not
later than ...
Fluorite and antimony deposits of epithermal type occurring in the central
geosynclinal zone and the late Pishin - Makran trough are formed in the Late
Paleogene and Neogene time . In any case the Pishin antimony deposits are not
later than ...
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
...
Page 12
... 8 -- Late Pishin - Makran trough ; 9 - South Makran depression ; filled with
Upper - Neogene molasses ; 10 — Pre Deccan foredeep deposits : 11 -
Manganese associated with marine volcanogenous beds ; 12 — Chromite ; 13 -
Asbestos ; 14 ...
... 8 -- Late Pishin - Makran trough ; 9 - South Makran depression ; filled with
Upper - Neogene molasses ; 10 — Pre Deccan foredeep deposits : 11 -
Manganese associated with marine volcanogenous beds ; 12 — Chromite ; 13 -
Asbestos ; 14 ...
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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