Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 2
... over- lain by thick recent deposits . Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline rocks forming the Sargodha Shield are known . It is worth mentioning that one of the features of the geological ...
... over- lain by thick recent deposits . Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline rocks forming the Sargodha Shield are known . It is worth mentioning that one of the features of the geological ...
Page 8
... overlain by the Oligocene deposits of late Pishin- Makran trough , due to which the belt is limited in width . Moreover it is not excluded , that within a single chromite ore belt , such as it is supposed to be at the present time ...
... overlain by the Oligocene deposits of late Pishin- Makran trough , due to which the belt is limited in width . Moreover it is not excluded , that within a single chromite ore belt , such as it is supposed to be at the present time ...
Page 3
... overlain with a possible non - sequence by the Sembar formation of doubt- ful Upper Jurassic - Neocomian age . 2. The Callovian genera K. ( Bomburites ) and Paralcidia are reported for the first time from Pakistan . 3. The presence of a ...
... overlain with a possible non - sequence by the Sembar formation of doubt- ful Upper Jurassic - Neocomian age . 2. The Callovian genera K. ( Bomburites ) and Paralcidia are reported for the first time from Pakistan . 3. The presence of a ...
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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