Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 5
... place . These deposits are big lenses of high grade native sulphur from several to 30 meters in thickness . During ... place after the main folding when the closing of the geosynclinal regime begins and the uplift of the folded ...
... place . These deposits are big lenses of high grade native sulphur from several to 30 meters in thickness . During ... place after the main folding when the closing of the geosynclinal regime begins and the uplift of the folded ...
Page 9
... place of tectonic zones which are characterized by a diffe- rent type of development and their position in space is defined at present by the position of their structural borders . On the scheme attached ( Fig . 2 ) are clearly shown ...
... place of tectonic zones which are characterized by a diffe- rent type of development and their position in space is defined at present by the position of their structural borders . On the scheme attached ( Fig . 2 ) are clearly shown ...
Page 10
... place , and they are characterized by a clearly definite mineralization . 4. Usually the endogenous ore formations of each stage of development are located in space exactly within the limits of the corresponding ore belts , the ...
... place , and they are characterized by a clearly definite mineralization . 4. Usually the endogenous ore formations of each stage of development are located in space exactly within the limits of the corresponding ore belts , the ...
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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