Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 8
... distinguished , it is of a different structural position and is clearly confined to the deep marginal fractures bordering the Chagai median massif in the South . The second , the Pishin - Makran mercury - antimony ore belt is situated ...
... distinguished , it is of a different structural position and is clearly confined to the deep marginal fractures bordering the Chagai median massif in the South . The second , the Pishin - Makran mercury - antimony ore belt is situated ...
Page 9
... distinguished , and they are characterized by a strictly definite metallogeny . In the central geosynclinal trough zone at the early stage of geosynclinal development , the formation of manganese , barite - polymetallic and chromite de ...
... distinguished , and they are characterized by a strictly definite metallogeny . In the central geosynclinal trough zone at the early stage of geosynclinal development , the formation of manganese , barite - polymetallic and chromite de ...
Page 10
... distinguished ; at the same time each geosyncline has its own specific provincial metallogenic peculiarities . So , at an early stage of the Baluchistan geosynclinal development the chromite and barite mineralization was intensely mani ...
... distinguished ; at the same time each geosyncline has its own specific provincial metallogenic peculiarities . So , at an early stage of the Baluchistan geosynclinal development the chromite and barite mineralization was intensely mani ...
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Common terms and phrases
ammonite ammonite bed antimony argillaceous limestone bed Bajocian Baluchistan Baluchistan geosynclinal development barite Bathonian Belemnite bifurcating body chamber central geosynclinal trough Chagai median massif Chiltan limestone Choffatia chromite chromite deposits Cutch described specimen diadematus Waagen disconformably Dolikephalites endogenous deposits endogenous mineralization Fatmi felsic fluorite fluorite deposits fractured genus geosynclinal holotype Homoeoplanulites indet Indian Platform Indocephalites Locality.-Wam Tangi Lower Callovian Lower Callovian ammonite Macrocephalites magmatism magnetite Massive limestone Mazar Drik formation Mazar Drik limestone metallogeny microconch molybdenum Noetling Oligocene Paleogene Paralcidia Pishin Pleurocephalites polyphemus primary ribs pyritic pyritic argillaceous limestone regularities of distribution ribbing style rocks Sembar formation sequence shale shell side view skarn southern Spath specimens internal mould Stratigraphic Range.-Lower Callovian subgenus Survey of Pakistan Takatu limestone thin bedded limestone Tithonian trifurcate ultramafic intrusions Umbilical diameter umbilical wall umbilicus Upper venter volcanogenous Vredenburg 1909 Wam Tangi West Pakistan Whorl height whorl section whorl side Whorl thickness