Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 1
... situated to the South of 32 ° parallel , is closely connected with the Alpine geosynclinal belt of the Tethys , the largest transcontinental structure of the Earth's Crust , extending in the sub - latitudinal direction from the Straits ...
... situated to the South of 32 ° parallel , is closely connected with the Alpine geosynclinal belt of the Tethys , the largest transcontinental structure of the Earth's Crust , extending in the sub - latitudinal direction from the Straits ...
Page 5
... situated to the west of Hyderabad . The deposit seems to be of infiltration type . The most prominent of them is shown by an open fracture from 0.15 m to 0.5 m in width cutting horizontally lying Tertiary shell limestones . The walls of ...
... situated to the west of Hyderabad . The deposit seems to be of infiltration type . The most prominent of them is shown by an open fracture from 0.15 m to 0.5 m in width cutting horizontally lying Tertiary shell limestones . The walls of ...
Page 10
... situated between the Iran and Kurin depression . In the Maly Kavkaz , similar structures and types of de- posits are distinguished ; at the same time each geosyncline has its own specific provincial metallogenic peculiarities . So , at ...
... situated between the Iran and Kurin depression . In the Maly Kavkaz , similar structures and types of de- posits are distinguished ; at the same time each geosyncline has its own specific provincial metallogenic peculiarities . So , at ...
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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