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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 3
Manganese formations are most prominent in the south of the zone in Las Bela
region where they are often confined to the Cretaceous pillow lavas , among
which jasper layers with manganese oxides occur in contact with shales ( Siro ...
Manganese formations are most prominent in the south of the zone in Las Bela
region where they are often confined to the Cretaceous pillow lavas , among
which jasper layers with manganese oxides occur in contact with shales ( Siro ...
Page 5
The most prominent of them is shown by an open fracture from 0.15 m to 0.5 m in
width cutting horizontally lying Tertiary shell limestones . The walls of the fracture
are covered with crystals of columnar celestite , forming symmetrical zones ...
The most prominent of them is shown by an open fracture from 0.15 m to 0.5 m in
width cutting horizontally lying Tertiary shell limestones . The walls of the fracture
are covered with crystals of columnar celestite , forming symmetrical zones ...
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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