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Page 1
Problems of metallogeny of West Pakistan have not been discussed in geological
literature . Probably ... These investigations essentially exhaust all the works
where the analysis of metallogenic development of West Pakistan had been
given .
Problems of metallogeny of West Pakistan have not been discussed in geological
literature . Probably ... These investigations essentially exhaust all the works
where the analysis of metallogenic development of West Pakistan had been
given .
Page 9
MAIN CONCLUSIONS 1. Features of endogenous metallogeny of the southern
part of West Pakistan are principally defined by eugeosynclinal character of the
Baluchistan geosynclinal development with the evolution of which , the origin of ...
MAIN CONCLUSIONS 1. Features of endogenous metallogeny of the southern
part of West Pakistan are principally defined by eugeosynclinal character of the
Baluchistan geosynclinal development with the evolution of which , the origin of ...
Page 10
As to the character of magmatism and endogenous metallogeny , the concerned
region chiefly embracing the ... types of deposits are distinguished ; at the same
time each geosyncline has its own specific provincial metallogenic peculiarities .
As to the character of magmatism and endogenous metallogeny , the concerned
region chiefly embracing the ... types of deposits are distinguished ; at the same
time each geosyncline has its own specific provincial metallogenic peculiarities .
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Common terms and phrases
Alpine ammonite ammonite bed antimony argillaceous Arkell associated Baluchistan geosynclinal barite Bela Belemnite belt body chamber Bomburites border central geosynclinal trough Chagai median massif characteristic characterized Chiltan limestone Choffatia chromite chromite deposits closely comparable complex confined connected consider copper correlation Cretaceous Cutch described diameter Dimensions distinguished distribution early effusives endogenous deposits endogenous mineralization extending fauna figured folded followed formation formed fractured geological Geological Survey geosynclinal development Jurassic Kheraiceras known late limits Lower Callovian Macrocephalites magmatism manifestations Mazar Drik metallogeny Middle molybdenum Nakus Neocomian Noetling occur Oligocene origin outline Paralcidia Pishin-Makran Platform possible present pyritic region regularities relation represented ribs rocks sedimentation sequence shale shell skarn southern Spath specimen stage structures submarine Survey of Pakistan thickness thin took ultramafic intrusions umbilical unit Upper Waagen Wam Tangi West Pakistan whorl section whorl side widely zone