Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 1
... widely developed within this zone , the total thickness of which reaches to 7 km . In the lower parts of the section of geosynclinal complexes , rocks of the Permian age are known ( which grades into the Triassic rocks ) . In the ...
... widely developed within this zone , the total thickness of which reaches to 7 km . In the lower parts of the section of geosynclinal complexes , rocks of the Permian age are known ( which grades into the Triassic rocks ) . In the ...
Page 3
... widely developed . There is a distinct relation between the massifs of ultramafic rocks with large zones of dislocations ; at the same time one can observe that the largest massifs are located in the regions of transections of ...
... widely developed . There is a distinct relation between the massifs of ultramafic rocks with large zones of dislocations ; at the same time one can observe that the largest massifs are located in the regions of transections of ...
Page 4
... widely displayed . The oldest among them are small chromite deposits located in the ultramafic intrusions of Ras - Koh ridge . These intrusions are confined to the tec- tonic suture separating the median massif from the geosynclinal ...
... widely displayed . The oldest among them are small chromite deposits located in the ultramafic intrusions of Ras - Koh ridge . These intrusions are confined to the tec- tonic suture separating the median massif from the geosynclinal ...
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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