Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 3
... fractured zones in the Jurassic limestone . The thickness of ore bodies varies from 1.0 m to 1.5 m . The strike of the veins is not well traced . Individual ore bodies appear to stretch hundreds of meters . Ore bodies are supposed to ...
... fractured zones in the Jurassic limestone . The thickness of ore bodies varies from 1.0 m to 1.5 m . The strike of the veins is not well traced . Individual ore bodies appear to stretch hundreds of meters . Ore bodies are supposed to ...
Page 4
... fractured intrusions which are usually followed by insignificant skarn type iron ore mineralization . To those deposits belongs Bandegan deposit in Ras - Koh mountains situated 70 km east of Dalbandin . The deposit is represented by a ...
... fractured intrusions which are usually followed by insignificant skarn type iron ore mineralization . To those deposits belongs Bandegan deposit in Ras - Koh mountains situated 70 km east of Dalbandin . The deposit is represented by a ...
Page 9
... fractured intrusions , often have vast deposits . Therefore , due to favourable regional structural factors and direct signs of mineralizstion , we have outlined within the Chagai median massif , a copper - molybdenum ore as belt as a ...
... fractured intrusions , often have vast deposits . Therefore , due to favourable regional structural factors and direct signs of mineralizstion , we have outlined within the Chagai median massif , a copper - molybdenum ore as belt as a ...
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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