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The Alpine structures are characterised by prevailing sub - latitudinal directions
with the contrast of transversal meridional structures in the eastern part . The
main regional geological features of the area are outlined and a summary on the
...
The Alpine structures are characterised by prevailing sub - latitudinal directions
with the contrast of transversal meridional structures in the eastern part . The
main regional geological features of the area are outlined and a summary on the
...
Page 1
The Alpine structures of this belt as a whole are characterized by prevailing
sublatitudinal directions and only in the ... and is distinctly traced in the
meridional direction from Karachi to Quetta and further in the regions of North
Waziristan .
The Alpine structures of this belt as a whole are characterized by prevailing
sublatitudinal directions and only in the ... and is distinctly traced in the
meridional direction from Karachi to Quetta and further in the regions of North
Waziristan .
Page 2
The maj . ority of the prominent dislocations with a break in continuity coincides
with the direction of folded structures and has a meridional or north - eastern
trend . After rather a short outline of the main regional geological features of the ...
The maj . ority of the prominent dislocations with a break in continuity coincides
with the direction of folded structures and has a meridional or north - eastern
trend . After rather a short outline of the main regional geological features of the ...
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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