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ABSTRACT The area is closely connected with the Alpine geosynclinal belt of the
Tethys , forming distinctly lineated folded belts , outlining numerous median
massifs and projections of platforms . The Alpine structures are characterised by
...
ABSTRACT The area is closely connected with the Alpine geosynclinal belt of the
Tethys , forming distinctly lineated folded belts , outlining numerous median
massifs and projections of platforms . The Alpine structures are characterised by
...
Page 1
Within the Baluchistan Tethys branch some tectonic units are prominent , which
are characterized by specific geological history of development and
metallogency . According to K.N. Kravchenko , B. A. Sokolov and others ( 1965 ) ,
five ...
Within the Baluchistan Tethys branch some tectonic units are prominent , which
are characterized by specific geological history of development and
metallogency . According to K.N. Kravchenko , B. A. Sokolov and others ( 1965 ) ,
five ...
Page 2
... of West Pakistan , defining all the architecture of the meridional Baluchistan
branch of the Tethys . In each of these zones one can distinguish , with a more or
less degree of validity , structures of a lower order . However detailed regional ...
... of West Pakistan , defining all the architecture of the meridional Baluchistan
branch of the Tethys . In each of these zones one can distinguish , with a more or
less degree of validity , structures of a lower order . However detailed regional ...
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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