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Page 2
Throughout the Oligocene there is a sharp change in the character of
sedimentation , that took place in shallow seas and ... shallow marine sediments
were deposited and in the Cretaceous time it was the arena of an intense
development of ...
Throughout the Oligocene there is a sharp change in the character of
sedimentation , that took place in shallow seas and ... shallow marine sediments
were deposited and in the Cretaceous time it was the arena of an intense
development of ...
Page 6
TABLE - I Structural zones 1 2 3 4 5 6 Sedimentation Weekly cemented
conglomerates , sandstones and schists . v Sedimentation Mainly thick carbonate
eds . Schists , sandstones. SCHEME OF DEVELOPMENT OF ENDOGENOUS ...
TABLE - I Structural zones 1 2 3 4 5 6 Sedimentation Weekly cemented
conglomerates , sandstones and schists . v Sedimentation Mainly thick carbonate
eds . Schists , sandstones. SCHEME OF DEVELOPMENT OF ENDOGENOUS ...
Page 7
v Sedimentation Mainly thick carbonate eds . Schists , sandstones , rarer limes
tones interbedded with volcanic rocks . ABOUT ORE BELTS Comprehensive
analysis of the regularities of distribution. border with Middle ( Principal folded
phase ...
v Sedimentation Mainly thick carbonate eds . Schists , sandstones , rarer limes
tones interbedded with volcanic rocks . ABOUT ORE BELTS Comprehensive
analysis of the regularities of distribution. border with Middle ( Principal folded
phase ...
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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