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1 1 | 1E 다 . 1 | INTRODUCTION The southern part of West Pakistan has a
complex.
1 1 | 1E 다 . 1 | INTRODUCTION The southern part of West Pakistan has a
complex.
Page 1
INTRODUCTION The southern part of West Pakistan has a complex geological
structure , the main features of which have not been terpreted 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 terpreted yet and their
thorough study is a matter of future investigations . Still less are known about the
...
Page 2
In the south this median block is cut by complex zones of marginal fractures from
the Pishin - Makran trough . Large tectonic dislocations in many regions are also
marked along the border of the main geosynclinal trough and adjacent structural
...
In the south this median block is cut by complex zones of marginal fractures from
the Pishin - Makran trough . Large tectonic dislocations in many regions are also
marked along the border of the main geosynclinal trough and adjacent structural
...
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Common terms and phrases
analysis antimony associated Baluchistan geosyncline barite bearing Bela region belt bodies border central geosynclinal trough Chagai median massif characteristic characterized chromite deposits clearly closely complex composed confined connected consider consideration copper copper-molybdenum Cretaceous definite direction dislocations distinguishing Early effusives endogenous deposits endogenous mineralization epithermal evidently extends felsic fluorite fluorite deposits folded folded structures formation formed fracture zones fractured geological geosynclinal development Hindubagh Indian Platform iron known largest late lenses limestones limits Magmatism magnetite major manganese manifestations marginal marked meridional metallogeny mineral deposits molybdenum Neogene northern observe occur Oligocene origin outlined Paleogene period Pishin position possible present processes prominent region regularities of distribution relation represented rocks Scheme sedimentation sequences significance situated skarn southern stage structural zones structures studied tectonic terrestrial territory Tethys thickness took traced ultramafic intrusions ultramafic rocks veins volcanic volcanogenous West Pakistan widely developed zone