From inside the book
Results 1-3 of 7
Page 8
One can distinguish here three ore belts , their borders coinciding with the
position of the main structural zones : ( a ) chromite ore belt confined to the axial
part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the ...
One can distinguish here three ore belts , their borders coinciding with the
position of the main structural zones : ( a ) chromite ore belt confined to the axial
part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the ...
Page 10
The second exception is , that the fluorite deposits originating in the later stage
are located in the region of chromite but not in the mercury - antimony ore belt
though they are of the same age . 5. It is necessary to emphasize that the
chemical ...
The second exception is , that the fluorite deposits originating in the later stage
are located in the region of chromite but not in the mercury - antimony ore belt
though they are of the same age . 5. It is necessary to emphasize that the
chemical ...
Page 12
... terrestrial effusives , skarn hydrothernmal ; 17 — Copper ( chalcopyrite - skarn
and hydrothermal ) and copper - molybdenum ( hydrothermal ) ; 18– Lead - zinc ,
hydrothermal ; 19 — Epithermal fluorite ; 20 - Antimony ; 21 - Native sulphur .
... terrestrial effusives , skarn hydrothernmal ; 17 — Copper ( chalcopyrite - skarn
and hydrothermal ) and copper - molybdenum ( hydrothermal ) ; 18– Lead - zinc ,
hydrothermal ; 19 — Epithermal fluorite ; 20 - Antimony ; 21 - Native sulphur .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Other editions - View all
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