Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 4
... thin stringers . Ores are of a simple compositon , the principal minerals are finegrained chalcedonous quartz and antimony . A characteristic feature of the antimony mineralization is its being confined to complex and old faults . It ...
... thin stringers . Ores are of a simple compositon , the principal minerals are finegrained chalcedonous quartz and antimony . A characteristic feature of the antimony mineralization is its being confined to complex and old faults . It ...
Page
... thin ferruginous reddish brown clay towards the base . Thickness 1 to 3 feet approximately . DISCONFORMITY A ... ( thin bedded limestone and shale equivalent to Mazar Drik lime- stone ) in the Sarwan area and assigned to the Callovian ...
... thin ferruginous reddish brown clay towards the base . Thickness 1 to 3 feet approximately . DISCONFORMITY A ... ( thin bedded limestone and shale equivalent to Mazar Drik lime- stone ) in the Sarwan area and assigned to the Callovian ...
Page 1
... thin bedded limestone & shale . Shrinab formation Loralai Ist dark , thin bedded Lst dark , thin bedded limestone and shale with sandstone . Bose considered to be Permion Kingriall Formation Tridion Formation Mianwali Formation Paro ...
... thin bedded limestone & shale . Shrinab formation Loralai Ist dark , thin bedded Lst dark , thin bedded limestone and shale with sandstone . Bose considered to be Permion Kingriall Formation Tridion Formation Mianwali Formation Paro ...
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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