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Page 1
Still less are known about the regularities of distribution of the endogenous
mineral deposits in this region , which are represented by a sufficiently broad
spectrum of ore showings . Problems of metallogeny of West Pakistan have not
been ...
Still less are known about the regularities of distribution of the endogenous
mineral deposits in this region , which are represented by a sufficiently broad
spectrum of ore showings . Problems of metallogeny of West Pakistan have not
been ...
Page 2
The latter are widely developed in the Chagai median massif and are practically
absent in the zone of central ( axial ) geosynclinal trough where they are only
represented by small massifs of plagiogranites . For the Pishin - Makran
secondary ...
The latter are widely developed in the Chagai median massif and are practically
absent in the zone of central ( axial ) geosynclinal trough where they are only
represented by small massifs of plagiogranites . For the Pishin - Makran
secondary ...
Page 9
Copper occurrences within this structure are most abundant , which are
represented by skarn and hydrothermal types , molybdenum mineralization being
at present of minor significance . Within the belt , numerous iron ore occurrences
are ...
Copper occurrences within this structure are most abundant , which are
represented by skarn and hydrothermal types , molybdenum mineralization being
at present of minor significance . Within the belt , numerous iron ore occurrences
are ...
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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
Bibliographic information
| Title | Memoirs of the Geological Survey of Pakistan, Volumes 7-8 Memoirs of the Geological Survey of Pakistan, Geological Survey of Pakistan Memoirs of the Geological Survey of Pakistan: Palaeontologia Pakistanica |
| Contributor | Geological Survey of Pakistan |
| Publisher | The Survey, 1969 |
| Original from | the University of Michigan |
| Digitized | 14 Feb 2008 |
| Export Citation | BiBTeX EndNote RefMan |