From inside the book
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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 9
The upper age limit of mineralization is not fixed but probably it can be of the
Oligocene age as , since that t'me , signs of active intrusive activity on the
discussed region of West Pakistan have not been stated , The marked major
regional ...
The upper age limit of mineralization is not fixed but probably it can be of the
Oligocene age as , since that t'me , signs of active intrusive activity on the
discussed region of West Pakistan have not been stated , The marked major
regional ...
Page
Fatmi , A. N. 1968 The paleontology and stratigraphy of the Mesozoic rocks of
Western Kohat Kala Chitta , Hazara and the Trans Indus Salt Range , West
Pakistan . Ph.D. Thesis University of Wales 1-409 , 47 pls . Hunting Survey
Corporation ...
Fatmi , A. N. 1968 The paleontology and stratigraphy of the Mesozoic rocks of
Western Kohat Kala Chitta , Hazara and the Trans Indus Salt Range , West
Pakistan . Ph.D. Thesis University of Wales 1-409 , 47 pls . Hunting Survey
Corporation ...
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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