Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 4
... characteristic ones for the central Baluchistan geosynclinal zone . These deposits were formed in Late Cretaceous - Upper Paleogene time . Fluorite deposits are endogenous formations of a more younger age and they evidently originated ...
... characteristic ones for the central Baluchistan geosynclinal zone . These deposits were formed in Late Cretaceous - Upper Paleogene time . Fluorite deposits are endogenous formations of a more younger age and they evidently originated ...
Page 5
... characteristic especially taking into consideration its relation with volcanogenous complexes . No less characteristic is the copper mineralization which is followed in some cases by the molybdenum one . The youngest endogenous mineral ...
... characteristic especially taking into consideration its relation with volcanogenous complexes . No less characteristic is the copper mineralization which is followed in some cases by the molybdenum one . The youngest endogenous mineral ...
Page 10
... characteristic and endogenous mineral concentrations related with felsic and ultrafelsic granites are not typical . 7. As to the character of magmatism and endogenous metallogeny , the concerned region chiefly embracing the Baluchistan ...
... characteristic and endogenous mineral concentrations related with felsic and ultrafelsic granites are not typical . 7. As to the character of magmatism and endogenous metallogeny , the concerned region chiefly embracing the Baluchistan ...
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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