Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
From inside the book
Results 1-3 of 16
Page 2
... is more complex ; breccia zones are commonly developed along it where one can observe different relation between ultramafics and 2 The Zone of the Central Geosynclinal Trough Abstract Introduction Pishin-Makran Zone Chagai Median Massif.
... is more complex ; breccia zones are commonly developed along it where one can observe different relation between ultramafics and 2 The Zone of the Central Geosynclinal Trough Abstract Introduction Pishin-Makran Zone Chagai Median Massif.
Page 4
... ZONE Endogenous deposits are practically absent in this zone which is a large scale late trough mainly composed of Oli- gocene flysch - like sequence . Only in the extreme north of the zone , in the Pishin town area , poorly studied ...
... ZONE Endogenous deposits are practically absent in this zone which is a large scale late trough mainly composed of Oli- gocene flysch - like sequence . Only in the extreme north of the zone , in the Pishin town area , poorly studied ...
Page 5
... region is reflected in the table enclosed , where data of develop- ment of different types of endogenous deposits are summarized , ( Table - I ) . 6 TABLE - I Structural zones 1 2 3 5 5 The Pre-Deccan Foredeep Zone The Indian Platform Zone.
... region is reflected in the table enclosed , where data of develop- ment of different types of endogenous deposits are summarized , ( Table - I ) . 6 TABLE - I Structural zones 1 2 3 5 5 The Pre-Deccan Foredeep Zone The Indian Platform Zone.
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