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Page 2
In the limits of the Baluchistan geosyncline , a special position is occupied by the
Chagai median massif , which is the southern part of a large median structure
separating the southern and northern branches of the Tethys ( Tvalchrelidze ,
1964 ) ...
In the limits of the Baluchistan geosyncline , a special position is occupied by the
Chagai median massif , which is the southern part of a large median structure
separating the southern and northern branches of the Tethys ( Tvalchrelidze ,
1964 ) ...
Page 8
Within its limits the singling out of ultramafic massifs and chrome deposits is
marked in three zones : Waziristan , Hindubagh and Las Bela zone . For the
Hindubagh zone which has a sub - latitudinal trend , a pronounced confinement
of ...
Within its limits the singling out of ultramafic massifs and chrome deposits is
marked in three zones : Waziristan , Hindubagh and Las Bela zone . For the
Hindubagh zone which has a sub - latitudinal trend , a pronounced confinement
of ...
Page 10
closely connected with the Baluchistan geosynclinal development , it is in fact
beyond its limits as if going away laterally and locating itself among rigid
structures of geosynclinal enclosing rock . The formation of the supposed
mercuryantimony ...
closely connected with the Baluchistan geosynclinal development , it is in fact
beyond its limits as if going away laterally and locating itself among rigid
structures of geosynclinal enclosing rock . The formation of the supposed
mercuryantimony ...
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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 |