Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
From inside the book
Results 1-3 of 4
Page
T ABSTRACT The area is closely connected with the Alpine geosynclinal belt of the Tethys , forming distinctly lineated folded belts , outlining numerous median massifs and projections of platforms . The Alpine structures are ...
T ABSTRACT The area is closely connected with the Alpine geosynclinal belt of the Tethys , forming distinctly lineated folded belts , outlining numerous median massifs and projections of platforms . The Alpine structures are ...
Page 1
... Tethys . In late 1967 , the author had an opportunity to visit the southern part of West Pakistan and to make some ... Tethys , the largest transcontinental structure of the Earth's Crust , extending in the sub - latitudinal direction ...
... Tethys . In late 1967 , the author had an opportunity to visit the southern part of West Pakistan and to make some ... Tethys , the largest transcontinental structure of the Earth's Crust , extending in the sub - latitudinal direction ...
Page 2
... Tethys . In each of these zones one can distinguish , with a more or less degree of validity , structures of a lower order . However detailed regional demarcation is very difficult because of poor geological study of West Pakistan ...
... Tethys . In each of these zones one can distinguish , with a more or less degree of validity , structures of a lower order . However detailed regional demarcation is very difficult because of poor geological study of West Pakistan ...
Other editions - View all
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