Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
From inside the book
Results 1-3 of 5
Page 5
... exposed by narrow canyons on the bottom of which mineral sources pour out . In these springs the formation of native sulphur is now taking place . These deposits are big lenses of high grade native sulphur from several to 30 meters in ...
... exposed by narrow canyons on the bottom of which mineral sources pour out . In these springs the formation of native sulphur is now taking place . These deposits are big lenses of high grade native sulphur from several to 30 meters in ...
Page
... exposed the ammonite bed which follows the Chiltan limestone with a marked disconformity which is indicated by the ferruginous clay at the base of the ammonite bed and by the uneven lateritic top surface of the Chiltan limestone . The ...
... exposed the ammonite bed which follows the Chiltan limestone with a marked disconformity which is indicated by the ferruginous clay at the base of the ammonite bed and by the uneven lateritic top surface of the Chiltan limestone . The ...
Page 3
... exposed below the Macrocephalites rocks in the Mazar Drik section are equivalent to the Loralai limestone . If his assignment of Lower Jurassic age for the Lora lai limestone is correct , a time gap is indicated between the two ...
... exposed below the Macrocephalites rocks in the Mazar Drik section are equivalent to the Loralai limestone . If his assignment of Lower Jurassic age for the Lora lai limestone is correct , a time gap is indicated between the two ...
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