From inside the book
Results 1-3 of 7
Page 1
INTRODUCTION The southern part of West Pakistan has a complex geological
structure , the main features of which have not been interpreted yet and their
thorough study is a matter of future investigations . Still less are known about the
...
INTRODUCTION The southern part of West Pakistan has a complex geological
structure , the main features of which have not been interpreted yet and their
thorough study is a matter of future investigations . Still less are known about the
...
Page 2
One should evidently refer the initial stage of the Baluchistan geosyncline to the
late Paleozoic period when , in the marginal part of the Indian Platform a complex
system of meridional deep faults originated , breaking up the consolidated ...
One should evidently refer the initial stage of the Baluchistan geosyncline to the
late Paleozoic period when , in the marginal part of the Indian Platform a complex
system of meridional deep faults originated , breaking up the consolidated ...
Page 4
A characteristic feature of the antimony mineralization is its being confined to
complex and old faults . It should be noted that on the extension of Pishin zone of
fractures which control the distribution of antimony mineralization , some mercury
...
A characteristic feature of the antimony mineralization is its being confined to
complex and old faults . It should be noted that on the extension of Pishin zone of
fractures which control the distribution of antimony mineralization , some mercury
...
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 |