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Page 3
In general , ultramafic intrusions and chromite deposits associated with them and
ore manifestations are characteristically confined to the central trough of the
Baluchistan geosyncline within which geosynclinal carbonate complexes and ...
In general , ultramafic intrusions and chromite deposits associated with them and
ore manifestations are characteristically confined to the central trough of the
Baluchistan geosyncline within which geosynclinal carbonate complexes and ...
Page 8
ABOUT ORE BELTS Comprehensive analysis of the regularities of distribution of
the endogenous deposits and the geological ... Ultramafic intrusions and
chromite deposits are chiefly concentrated in the northern part of the belt
whereas in the ...
ABOUT ORE BELTS Comprehensive analysis of the regularities of distribution of
the endogenous deposits and the geological ... Ultramafic intrusions and
chromite deposits are chiefly concentrated in the northern part of the belt
whereas in the ...
Page 10
The first is due to the appearance of small chromite deposits in Ras Koh range ,
which are beyond the chromite ore belt , in the tectonic suture bordering the
Chagai median messifs in the south . The second exception is , that the fluorite ...
The first is due to the appearance of small chromite deposits in Ras Koh range ,
which are beyond the chromite ore belt , in the tectonic suture bordering the
Chagai median messifs in the south . The second exception is , that the fluorite ...
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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 |