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Page 2
The most eastern regions of the discussed territory belong to the Indian Platform ,
the structures of which are overlain by thick recent ... Unfortunately , up - till now
many cardinal points of the geological development of the region remain vague .
The most eastern regions of the discussed territory belong to the Indian Platform ,
the structures of which are overlain by thick recent ... Unfortunately , up - till now
many cardinal points of the geological development of the region remain vague .
Page 3
The upper age limit of the ultramafic intrusions of the Hindubagh region is of the
Eocene age . This conclusion is due to the fact that limestones containing fauna
of this age obviously superimpose the weathered surface of the ultramafic rocks .
The upper age limit of the ultramafic intrusions of the Hindubagh region is of the
Eocene age . This conclusion is due to the fact that limestones containing fauna
of this age obviously superimpose the weathered surface of the ultramafic rocks .
Page 8
Distinguishing such regional ore bearing structures has been done , to a great
extent provisionally , which is first of all due to ... belt whereas in the southern part
of the Las Bela region barite and barite - galena mineralization is most important .
Distinguishing such regional ore bearing structures has been done , to a great
extent provisionally , which is first of all due to ... belt whereas in the southern part
of the Las Bela region barite and barite - galena mineralization is most important .
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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 |