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Page 3
... massifs are located in the regions of transections of meridional and latitudinal
fractures ( Hindubagh , North Waziristan ) ... represented by a fluorite and
fluoritearbonate series of veins confined to the fractured zones in the Jurassic
limestone .
... massifs are located in the regions of transections of meridional and latitudinal
fractures ( Hindubagh , North Waziristan ) ... represented by a fluorite and
fluoritearbonate series of veins confined to the fractured zones in the Jurassic
limestone .
Page 5
It is necessary to emphasize the copper , molybdenum and lead deposits
occurrences associate with fractured intrusions of moderately felsic granitoids
and diorites within the Chagai median massif . Small iron deposits of skarn type
are also ...
It is necessary to emphasize the copper , molybdenum and lead deposits
occurrences associate with fractured intrusions of moderately felsic granitoids
and diorites within the Chagai median massif . Small iron deposits of skarn type
are also ...
Page 9
... the Chagai median massif within which as mentioned above , fracture
intrusions of intermediate to alkaline rocks followed by ... peripheral geosynclinal
parts showing terrest - ial volcanism and fractured intrusions , often have vast
deposits .
... the Chagai median massif within which as mentioned above , fracture
intrusions of intermediate to alkaline rocks followed by ... peripheral geosynclinal
parts showing terrest - ial volcanism and fractured intrusions , often have vast
deposits .
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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