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Page 24
The Wam Tangi ammonite fauna resembles strongly the Macrocephalites and
Choffatia fauna described by Noetling ( 1897 ) from Mazari Drik , Baluchistan .
Arkell ( 1956 ) , reviewing the fauna , places it in the Macrocephalus Zone , and ...
The Wam Tangi ammonite fauna resembles strongly the Macrocephalites and
Choffatia fauna described by Noetling ( 1897 ) from Mazari Drik , Baluchistan .
Arkell ( 1956 ) , reviewing the fauna , places it in the Macrocephalus Zone , and ...
Page 10
The Wam Tan i ammon't strOngly the Macrocephalites and Choflqtia fauna
described by Noetling ( 1897) fromg Mazari Osifgmlliilrngiriggli'is Arkell (1956),
reviewing the fauna, places it in the Macrocephalus Zone, and considers it to
have ...
The Wam Tan i ammon't strOngly the Macrocephalites and Choflqtia fauna
described by Noetling ( 1897) fromg Mazari Osifgmlliilrngiriggli'is Arkell (1956),
reviewing the fauna, places it in the Macrocephalus Zone, and considers it to
have ...
Page
Ph.D. Thesis University of Wales 1-409 , 47 pls . Hunting Survey Corporation Ltd.
1960 Reconnaissance Geology of part of West Pakistan , Toronto , Canada .
Noctling , F. 1897 The Jurassic fauna ; The fauna of the Kellaways of Mazar Drik .
Ph.D. Thesis University of Wales 1-409 , 47 pls . Hunting Survey Corporation Ltd.
1960 Reconnaissance Geology of part of West Pakistan , Toronto , Canada .
Noctling , F. 1897 The Jurassic fauna ; The fauna of the Kellaways of Mazar Drik .
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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