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Page 2
In general the Baluchistan geosyncline is characterized by a weak manifestation
of intrusive magmatism and rather subordinate significance of granitoidal rocks
with extremely constrasting display of derivative ultramafic and mafic magmas .
In general the Baluchistan geosyncline is characterized by a weak manifestation
of intrusive magmatism and rather subordinate significance of granitoidal rocks
with extremely constrasting display of derivative ultramafic and mafic magmas .
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
Distinguishing such regional ore bearing structures has been done , to a great
extent provisionally , which is first of all due to the lack of deposits or even ore
manifestations of definite mineral deposits at the present time . Their discovery is
...
Distinguishing such regional ore bearing structures has been done , to a great
extent provisionally , which is first of all due to the lack of deposits or even ore
manifestations of definite mineral deposits at the present time . Their discovery is
...
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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 |