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Page 5
The walls of the fracture are covered with crystals of columnar celestite , forming
symmetrical zones which are replaced to the centre of the cavity by zones of
sintered banded carbonate , bearing traces of origin from descending solutions .
The walls of the fracture are covered with crystals of columnar celestite , forming
symmetrical zones which are replaced to the centre of the cavity by zones of
sintered banded carbonate , bearing traces of origin from descending solutions .
Page 8
... within the belt should attract our greatest attention as in case of the presence of
direct ore indications ( the presence of fractures , disseminated mineralization )
which may be very favourable for the origin of major metasomatic ore deposits .
... within the belt should attract our greatest attention as in case of the presence of
direct ore indications ( the presence of fractures , disseminated mineralization )
which may be very favourable for the origin of major metasomatic ore deposits .
Page 9
... and in general , a rather prospective structure of that type of mineralization .
Intrusions followed by molybdenum and copper - mineralization break trough
Cretaceous and Eocene sediments that allows to correlate the time of their origin
...
... and in general , a rather prospective structure of that type of mineralization .
Intrusions followed by molybdenum and copper - mineralization break trough
Cretaceous and Eocene sediments that allows to correlate the time of their origin
...
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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 |