Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 2
... manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely constrasting ... manifestations are confined to the massif of ultramafics in the Hindubagh region . This massif has a complex ...
... manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely constrasting ... manifestations are confined to the massif of ultramafics in the Hindubagh region . This massif has a complex ...
Page 3
... manifestations are charac- teristically confined to the central trough of the Baluchistan geosyncline within which geosynclinal carbonate complexes and submarine effusives are widely developed . There is a distinct relation between the ...
... manifestations are charac- teristically confined to the central trough of the Baluchistan geosyncline within which geosynclinal carbonate complexes and submarine effusives are widely developed . There is a distinct relation between the ...
Page 8
... manifestations of definite mineral deposits at the present time . Their discovery is however quite possible . Besides , in some ore belts one or another type of prospective mineralization , which at present Is not dominating there , is ...
... manifestations of definite mineral deposits at the present time . Their discovery is however quite possible . Besides , in some ore belts one or another type of prospective mineralization , which at present Is not dominating there , is ...
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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