Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 4
... bearing fractures , antimony ores form lenses and mineralized zones of quartzose rocks . The thickness and length of individual zones attains 60 m and 500 m respectively ; they constitute an extended ore band , the total length of which ...
... bearing fractures , antimony ores form lenses and mineralized zones of quartzose rocks . The thickness and length of individual zones attains 60 m and 500 m respectively ; they constitute an extended ore band , the total length of which ...
Page 5
... bearing traces of origin from descerding solutions . According to K. D. Subbotin the zone of fracture with celestite mineralization can be traced for 9 kilometers ; however , the minera- lization depth is not great and does not exceed ...
... bearing traces of origin from descerding solutions . According to K. D. Subbotin the zone of fracture with celestite mineralization can be traced for 9 kilometers ; however , the minera- lization depth is not great and does not exceed ...
Page 8
... bearing structures has been done , to a great extent provisionally , which is first of all due to the lack of deposits or even ore manifestations of definite mineral deposits at the present time . Their discovery is however quite ...
... bearing structures has been done , to a great extent provisionally , which is first of all due to the lack of deposits or even ore manifestations of definite mineral deposits at the present time . Their discovery is however quite ...
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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