Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 4
... suture separating the median massif from the geosynclinal fold structures . The ultramafic intrusions are of frac tured nature and are strictly confined to the fracture zones . They are rather small , their thickness attains 15 to 50 m ...
... suture separating the median massif from the geosynclinal fold structures . The ultramafic intrusions are of frac tured nature and are strictly confined to the fracture zones . They are rather small , their thickness attains 15 to 50 m ...
Page 8
... sutured intrusions of peridotites with small chromite deposits are known . This subject requires an analysis of additional reliable data and cannot be definitely solved now . The recent reliable data allow with greater certainty to ...
... sutured intrusions of peridotites with small chromite deposits are known . This subject requires an analysis of additional reliable data and cannot be definitely solved now . The recent reliable data allow with greater certainty to ...
Page 10
... suture bordering the Chagai median messifs in the south . The second exception is , that the fluorite deposits originating in the later stage are located in the region . of chromite but not in the mercury - antimony ore belt though they ...
... suture bordering the Chagai median messifs in the south . The second exception is , that the fluorite deposits originating in the later stage are located in the region . of chromite but not in the mercury - antimony ore belt though they ...
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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