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Page 3
In one case , marble fragments are cemented by serpentinized ultramafic rocks ,
in others , the fragments of the later occur in the marbles . Sometimes one can
see such contradictory relations in one outcrop , which show a highly complex ...
In one case , marble fragments are cemented by serpentinized ultramafic rocks ,
in others , the fragments of the later occur in the marbles . Sometimes one can
see such contradictory relations in one outcrop , which show a highly complex ...
Page 4
These occur in the Oligocene sandstone - shale sequences and are confined to
major and extended zones of dislocations of north - east trend . Within ore
bearing fractures , antimony ores form lenses and mineralized zones of
quartzose rocks ...
These occur in the Oligocene sandstone - shale sequences and are confined to
major and extended zones of dislocations of north - east trend . Within ore
bearing fractures , antimony ores form lenses and mineralized zones of
quartzose rocks ...
Page 10
Only sometimes , some elements have through passage and occur in the
deposits of different stages . ... At present it is known that barite occurs in Pishin
antimony ores and cinnabar in barite deposits of Khuzdar region which is
supposed to ...
Only sometimes , some elements have through passage and occur in the
deposits of different stages . ... At present it is known that barite occurs in Pishin
antimony ores and cinnabar in barite deposits of Khuzdar region which is
supposed to ...
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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 |