Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 2
... limits of the Baluchistan geosyncline , a special position is occupied by the Chagai median massif , which is the southern part of a large median structure separating the southern and northern branches of the Tethys ( Tvalchre- lidze ...
... limits of the Baluchistan geosyncline , a special position is occupied by the Chagai median massif , which is the southern part of a large median structure separating the southern and northern branches of the Tethys ( Tvalchre- lidze ...
Page 8
... limits is of leading importance and most conspicuously outlined . There is all ground to believe that some part of chromite ore belt is overlain by the Oligocene deposits of late Pishin- Makran trough , due to which the belt is limited ...
... limits is of leading importance and most conspicuously outlined . There is all ground to believe that some part of chromite ore belt is overlain by the Oligocene deposits of late Pishin- Makran trough , due to which the belt is limited ...
Page 10
... limits of the corresponding ore belts , the formation of which takes place at a definite stage . At present , out of this general regularity , two pronounced exceptions are marked . The first is due to the appearance of small chromite ...
... limits of the corresponding ore belts , the formation of which takes place at a definite stage . At present , out of this general regularity , two pronounced exceptions are marked . The first is due to the appearance of small chromite ...
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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