Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 5
... 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 the first scores 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 the first scores of ...
Page 8
... of direct ore indications ( the presence of fractures , disseminated mineralization ) which may be very favourable for the origin of major metasomatic ore deposits . The third , copper - molybdenum ore belt is confined 8.
... of direct ore indications ( the presence of fractures , disseminated mineralization ) which may be very favourable for the origin of major metasomatic ore deposits . The third , copper - molybdenum ore belt is confined 8.
Page 9
... origin with the period of principal folding phase in the central geosynclinal trough . The upper age limit of mineralization is not fixed but probably it can be of the Oligocene age as , since that t'me , signs of active intrusive ...
... origin with the period of principal folding phase in the central geosynclinal trough . The upper age limit of mineralization is not fixed but probably it can be of the Oligocene age as , since that t'me , signs of active intrusive ...
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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