Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 2
... marked regularities of distribution of endogenous deposits and their genetic features it is possible to make a metallogenetic analysis of this region . One should evidently refer the initial stage of the Baluchistan geosyn- cline to the ...
... marked regularities of distribution of endogenous deposits and their genetic features it is possible to make a metallogenetic analysis of this region . One should evidently refer the initial stage of the Baluchistan geosyn- cline to the ...
Page 8
... marked , which fully corresponds to ore belts . One can distinguish here three ore belts , their borders coinciding with the position of the main structural zones : ( a ) chromite ore belt confined to the axial part of the Baluchistan ...
... marked , which fully corresponds to ore belts . One can distinguish here three ore belts , their borders coinciding with the position of the main structural zones : ( a ) chromite ore belt confined to the axial part of the Baluchistan ...
Page 10
... marked . The first is due to the appearance of small chromite deposits in Ras Koh range , which are beyond the chromite ore belt , in the tectonic suture bordering the Chagai median messifs in the south . The second exception is , that ...
... marked . The first is due to the appearance of small chromite deposits in Ras Koh range , which are beyond the chromite ore belt , in the tectonic suture bordering the Chagai median messifs in the south . The second exception is , that ...
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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