Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
From inside the book
Results 1-3 of 12
Page 2
... rocks are typical . In general the Baluchistan geosyncline is characterized by a weak manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely constrasting display of de- rivative ...
... rocks are typical . In general the Baluchistan geosyncline is characterized by a weak manifestation of intrusive magmatism and rather subordinate significance of granitoidal rocks with extremely constrasting display of de- rivative ...
Page 3
... rocks . According to these data the time of formation of chromite mineralization within the northern part of the Baluchis- tan geosyncline is of Late Cretaceous - Paleocene age . The instrusions of ultramafic rocks in the Hindubagh ...
... rocks . According to these data the time of formation of chromite mineralization within the northern part of the Baluchis- tan geosyncline is of Late Cretaceous - Paleocene age . The instrusions of ultramafic rocks in the Hindubagh ...
Page 3
... rocks is carried out , their relationship will remain conjectural . This confusion , however , brings out one fact that in Baluchistan rocks of Lower Callovian , Bathonian and possibly Bajocian , are not uniformly distributed and that ...
... rocks is carried out , their relationship will remain conjectural . This confusion , however , brings out one fact that in Baluchistan rocks of Lower Callovian , Bathonian and possibly Bajocian , are not uniformly distributed and that ...
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