From inside the book
Results 1-3 of 5
Page 3
According to these data the time of formation of chromite mineralization within the
northern part of the Baluchistan geosyncline is of Late Cretaceous - Paleocene
age . The instrusions of The instrusions of ultramafic rocks in the Hindubagh ...
According to these data the time of formation of chromite mineralization within the
northern part of the Baluchistan geosyncline is of Late Cretaceous - Paleocene
age . The instrusions of The instrusions of ultramafic rocks in the Hindubagh ...
Page 7
Late . Paleozoic ( Perminan ) -MesozoicEarly Paleogene . Ultramafic intrusions (
perido- | Terrestrial continental mafic tites , dunites , rarer gabbro ) sub and felsic
effi usives marire volcanogenous comp ( Cretaceous ) lexes of porphyritic series
...
Late . Paleozoic ( Perminan ) -MesozoicEarly Paleogene . Ultramafic intrusions (
perido- | Terrestrial continental mafic tites , dunites , rarer gabbro ) sub and felsic
effi usives marire volcanogenous comp ( Cretaceous ) lexes of porphyritic series
...
Page 9
... a copper - molybdenum ore as belt as a regional and in general , a rather
prospective structure of that type of mineralization . Intrusions followed by
molybdenum and copper - mineralization break trough Cretaceous and Eocene
sediments ...
... a copper - molybdenum ore as belt as a regional and in general , a rather
prospective structure of that type of mineralization . Intrusions followed by
molybdenum and copper - mineralization break trough Cretaceous and Eocene
sediments ...
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
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