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Page 2
Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline
rocks forming the Sargodha Shield are known . It is worth mentioning that one of
the features of the geological structure of the territory concerned is rather a
limited ...
Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline
rocks forming the Sargodha Shield are known . It is worth mentioning that one of
the features of the geological structure of the territory concerned is rather a
limited ...
Page 4
Accoruingly chrome , manganese and barite ( with galena ) deposits which were
formed in the early stage of geosynclinal developinent are the most characteristic
ones for the central Baluchistan geosynclinal zone . These deposits were ...
Accoruingly chrome , manganese and barite ( with galena ) deposits which were
formed in the early stage of geosynclinal developinent are the most characteristic
ones for the central Baluchistan geosynclinal zone . These deposits were ...
Page 5
Ore lenses are located among a thick zone of crumpled and brecciated rhyolites .
M. I. Ahmed ( 1962 ) suggests that the mineralization is connected with
monzonite , outcropping to the south of the deposit . Upper age limit of the
considered ...
Ore lenses are located among a thick zone of crumpled and brecciated rhyolites .
M. I. Ahmed ( 1962 ) suggests that the mineralization is connected with
monzonite , outcropping to the south of the deposit . Upper age limit of the
considered ...
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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 |