Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 9
... development . Copper occurrences within this structure are most abundant ... geosynclinal parts showing terrestrial volcanism and fractured intrusions ... geosynclinal trough . The upper age limit of mineralization is not fixed but ...
... development . Copper occurrences within this structure are most abundant ... geosynclinal parts showing terrestrial volcanism and fractured intrusions ... geosynclinal trough . The upper age limit of mineralization is not fixed but ...
Page 10
closely connected with the Baluchistan geosynclinal development , it is in fact beyond its limits as if going away laterally and locating itself among rigid structures of geosynclinal enclosing rock . The formation of the supposed ...
closely connected with the Baluchistan geosynclinal development , it is in fact beyond its limits as if going away laterally and locating itself among rigid structures of geosynclinal enclosing rock . The formation of the supposed ...
Page 12
... geosyncline ; 23 - Chromite in fracture zon on the jointing of geosynclinal marginal troughs with median massifs ; 24 - Possible extension of Hindubag chromite zone ( II ) ; 25 - Zone of development of manganese , barite and barite ...
... geosyncline ; 23 - Chromite in fracture zon on the jointing of geosynclinal marginal troughs with median massifs ; 24 - Possible extension of Hindubag chromite zone ( II ) ; 25 - Zone of development of manganese , barite and barite ...
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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