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Page 19
A pre Lower Callovian disconformity is also established in Wam Tangi which
separates the Lower Callovian ammonite bed from the underlying Chiltan
Limestone of doubtful— ? LowerMiddle Jurassic age . The fauna compares
favourably with ...
A pre Lower Callovian disconformity is also established in Wam Tangi which
separates the Lower Callovian ammonite bed from the underlying Chiltan
Limestone of doubtful— ? LowerMiddle Jurassic age . The fauna compares
favourably with ...
Page 23
PREVIOUS WORK No ammonites of Jurassic age have been mentioned from this
area . Hunting Survey Corporation of Canada ( 1960 ) who geologically mapped
this territory on 1 " = 4 miles scale failed to establish any fossil evidence of the ...
PREVIOUS WORK No ammonites of Jurassic age have been mentioned from this
area . Hunting Survey Corporation of Canada ( 1960 ) who geologically mapped
this territory on 1 " = 4 miles scale failed to establish any fossil evidence of the ...
Page
REFERENCES Arkell , W. J. 1956 Jurassic Geology of the World XV 806 pp . 46
pls . Edinburgh and London . 1957 Mesozoic Ammonoidea . In Treatise on
Invertebrate Paleonlotogy Part L. Mollusca 4. Cephalopoda , Ammonoidea . ( Ed .
by ...
REFERENCES Arkell , W. J. 1956 Jurassic Geology of the World XV 806 pp . 46
pls . Edinburgh and London . 1957 Mesozoic Ammonoidea . In Treatise on
Invertebrate Paleonlotogy Part L. Mollusca 4. Cephalopoda , Ammonoidea . ( Ed .
by ...
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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