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Page 23
The ammonites occur in a thin bedded limestone and shale sequence named by
Arkell ( 1956 ) as Mazar Drik limestone and considered by Standard Vacuum Oil
Company ( J. R. Huth , Section No. 54 , 1960 ) as a 50 feet thick unit . Apparently
...
The ammonites occur in a thin bedded limestone and shale sequence named by
Arkell ( 1956 ) as Mazar Drik limestone and considered by Standard Vacuum Oil
Company ( J. R. Huth , Section No. 54 , 1960 ) as a 50 feet thick unit . Apparently
...
Page 24
with a 6 " to very thin ferruginous reddish brown clay towards the base .
Thickness 1 to 3 feet approximately . DISCONFORMITY A. Chiltan limestone ,
grey , medium grey , thick bedded limestone , colitic , fine to coarse texture in
beds with ...
with a 6 " to very thin ferruginous reddish brown clay towards the base .
Thickness 1 to 3 feet approximately . DISCONFORMITY A. Chiltan limestone ,
grey , medium grey , thick bedded limestone , colitic , fine to coarse texture in
beds with ...
Page 10
With a 6 to very thin ferruginous reddish browa clay towards the base. Thickness
1 to 3 feet approximately. . DISCONFORMITY A. Chiltan limestone, grey, medium
grey, thick bedded limestone, colitic, fine to coarse texture in beds with some ...
With a 6 to very thin ferruginous reddish browa clay towards the base. Thickness
1 to 3 feet approximately. . DISCONFORMITY A. Chiltan limestone, grey, medium
grey, thick bedded limestone, colitic, fine to coarse texture in beds with some ...
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Common terms and phrases
Alpine ammonite ammonite bed antimony argillaceous Arkell associated Baluchistan geosynclinal barite Bela Belemnite belt body chamber Bomburites border central geosynclinal trough Chagai median massif characteristic characterized Chiltan limestone Choffatia chromite chromite deposits closely comparable complex confined connected consider copper correlation Cretaceous Cutch described diameter Dimensions distinguished distribution early effusives endogenous deposits endogenous mineralization extending fauna figured folded followed formation formed fractured geological Geological Survey geosynclinal development Jurassic Kheraiceras known late limits Lower Callovian Macrocephalites magmatism manifestations Mazar Drik metallogeny Middle molybdenum Nakus Neocomian Noetling occur Oligocene origin outline Paralcidia Pishin-Makran Platform possible present pyritic region regularities relation represented ribs rocks sedimentation sequence shale shell skarn southern Spath specimen stage structures submarine Survey of Pakistan thickness thin took ultramafic intrusions umbilical unit Upper Waagen Wam Tangi West Pakistan whorl section whorl side widely zone
Bibliographic information
| Title | Memoirs of the Geological Survey of Pakistan, Volumes 7-8 Memoirs of the Geological Survey of Pakistan, Geological Survey of Pakistan Memoirs of the Geological Survey of Pakistan: Palaeontologia Pakistanica |
| Contributor | Geological Survey of Pakistan |
| Publisher | The Survey, 1969 |
| Original from | the University of Michigan |
| Digitized | 14 Feb 2008 |
| Export Citation | BiBTeX EndNote RefMan |