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Page 1
Attempts to interpret the features of endogenous mineralization of the southern
part of West Pakistan both in time and space from J. A. Bilibin's point of view on
the evolution of mineralization in the course of development of orogens have ...
Attempts to interpret the features of endogenous mineralization of the southern
part of West Pakistan both in time and space from J. A. Bilibin's point of view on
the evolution of mineralization in the course of development of orogens have ...
Page 5
No less characteristic is the copper mineralization which is followed in some
cases by the molybdenum one . The youngest endogenous mineral formations
within the Chagai median massif are the sulphur deposits ; they are confined to
vents ...
No less characteristic is the copper mineralization which is followed in some
cases by the molybdenum one . The youngest endogenous mineral formations
within the Chagai median massif are the sulphur deposits ; they are confined to
vents ...
Page 10
Thus in each stage of the Baluchistan geosynclinal development , the formation
of large regional orebearing structures of ore belt types took place , and they are
characterized by a clearly definite mineralization . 4. Usually the endogenous ore
...
Thus in each stage of the Baluchistan geosynclinal development , the formation
of large regional orebearing structures of ore belt types took place , and they are
characterized by a clearly definite mineralization . 4. Usually the endogenous ore
...
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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