Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 2
... geosynclinal trough submarine volcanic rocks are typical . In general the Baluchistan geosyncline is characterized by a weak manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely ...
... geosynclinal trough submarine volcanic rocks are typical . In general the Baluchistan geosyncline is characterized by a weak manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely ...
Page 9
... Baluchistan geosynclinal development with the evolution of which , the origin of magmatic , skarn and hydrothermal deposits of various mineral resources is connected . Typomorphic elements for the given region are : chrome , barite ...
... Baluchistan geosynclinal development with the evolution of which , the origin of magmatic , skarn and hydrothermal deposits of various mineral resources is connected . Typomorphic elements for the given region are : chrome , barite ...
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 ...
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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