From inside the book
Results 1-3 of 12
Page 1
The zone of central geosynclinal trough ( zone of Las - Bela - Hindubagh )
coincides with marginal development of calcareous , terrigenous and submarine
volcanogenous Mesozoic rock masses . It occupies the central axial position in
the ...
The zone of central geosynclinal trough ( zone of Las - Bela - Hindubagh )
coincides with marginal development of calcareous , terrigenous and submarine
volcanogenous Mesozoic rock masses . It occupies the central axial position in
the ...
Page 2
Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline
rocks forming the Sargodha Shield are known . It is worth mentioning that one of
the features of the geological structure of the territory concerned is rather a
limited ...
Only in the northeast of the zone , small outcrops of Pre - cambrian crystalline
rocks forming the Sargodha Shield are known . It is worth mentioning that one of
the features of the geological structure of the territory concerned is rather a
limited ...
Page 3
In one case , marble fragments are cemented by serpentinized ultramafic rocks ,
in others , the fragments of the later occur in the marbles . Sometimes one can
see such contradictory relations in one outcrop , which show a highly complex ...
In one case , marble fragments are cemented by serpentinized ultramafic rocks ,
in others , the fragments of the later occur in the marbles . Sometimes one can
see such contradictory relations in one outcrop , which show a highly complex ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Other editions - View all
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 |