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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
In general , for this kind of structure , iron mineralization is very characteristic
especially taking into consideration its relation with volcanogenous complexes .
No less characteristic is the copper mineralization which is followed in some
cases ...
In general , for this kind of structure , iron mineralization is very characteristic
especially taking into consideration its relation with volcanogenous complexes .
No less characteristic is the copper mineralization which is followed in some
cases ...
Page 10
For the territory of the southern part of West Pakistan the limited development of
granitic magmas is highly characteristic and endogenous mineral concentrations
related with felsic and ultrafelsic granites are not typical . 7. As to the character of
...
For the territory of the southern part of West Pakistan the limited development of
granitic magmas is highly characteristic and endogenous mineral concentrations
related with felsic and ultrafelsic granites are not typical . 7. As to the character of
...
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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 |