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Page 1
INTRODUCTION The southern part of West Pakistan has a complex geological
structure , the main features of which have ... folded structures of the Tethys
usually form distinctly lineated folded belts clearly outlining numerous median
massifs ...
INTRODUCTION The southern part of West Pakistan has a complex geological
structure , the main features of which have ... folded structures of the Tethys
usually form distinctly lineated folded belts clearly outlining numerous median
massifs ...
Page 2
The most eastern regions of the discussed territory belong to the Indian Platform ,
the structures of which are overlain by thick recent deposits . ... This structure
evidently forms a part of the Hercynian folded structures that are in Afghanistan .
The most eastern regions of the discussed territory belong to the Indian Platform ,
the structures of which are overlain by thick recent deposits . ... This structure
evidently forms a part of the Hercynian folded structures that are in Afghanistan .
Page 6
TABLE - I Structural zones 1 2 3 4 5 6 9 Sedimentation Weekly cemented
conglomerates , sandstones and schists . 7 Sedimentation Mainly ...
Consolidation of folded structures , increasing role of rupture dislocations .
Epithermal antimony ...
TABLE - I Structural zones 1 2 3 4 5 6 9 Sedimentation Weekly cemented
conglomerates , sandstones and schists . 7 Sedimentation Mainly ...
Consolidation of folded structures , increasing role of rupture dislocations .
Epithermal antimony ...
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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