Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 1
... consider some problems connected with the regularities of distribution of endogenous mineral deposits within the meridional Baluchistan branch of the Mediterranean geosynclinal belt or the Tethys . In late 1967 , the author had an ...
... consider some problems connected with the regularities of distribution of endogenous mineral deposits within the meridional Baluchistan branch of the Mediterranean geosynclinal belt or the Tethys . In late 1967 , the author had an ...
Page 2
... consider the sedimentation of the Baluchistan geosyn- cline to the troughs of eugeosynclinal type . The above mentioned five tectonic zones represent the largest structural units in the southern part of West Pakistan , defining all the ...
... consider the sedimentation of the Baluchistan geosyn- cline to the troughs of eugeosynclinal type . The above mentioned five tectonic zones represent the largest structural units in the southern part of West Pakistan , defining all the ...
Page 8
... consider that the distinguishing of such regional ore bearing structures , especially for poorly studied regions , like West Pakistan , is of great importance for the prognosis and the carry- ing out of current exploration programmes ...
... consider that the distinguishing of such regional ore bearing structures , especially for poorly studied regions , like West Pakistan , is of great importance for the prognosis and the carry- ing out of current exploration programmes ...
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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