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Scheme of development of endogenous mineralization of Baluchistan Alpine
folded region ( the southern part of West Pakistan ) pp . 6-7 . ILLUSTRATIONS
Fig . 1. - Scheme of distribution of main endogenous deposits in the Baluchistan ...
Scheme of development of endogenous mineralization of Baluchistan Alpine
folded region ( the southern part of West Pakistan ) pp . 6-7 . ILLUSTRATIONS
Fig . 1. - Scheme of distribution of main endogenous deposits in the Baluchistan ...
Page
ABSTRACT The area is closely connected with the Alpine geosynclinal belt of the
Tethys , forming distinctly lineated folded belts , outlining numerous median
massifs and projections of platforms . The Alpine structures are characterised by
...
ABSTRACT The area is closely connected with the Alpine geosynclinal belt of the
Tethys , forming distinctly lineated folded belts , outlining numerous median
massifs and projections of platforms . The Alpine structures are characterised by
...
Page 10
The closest to the Baluchistan geosyncline in respect of its metallogenous
features is the Alpine geosyncline of the Maly Kavkaz situated between the Iran
and Kurin depression . In the Maly Kavkaz , similar structures and types of
deposits are ...
The closest to the Baluchistan geosyncline in respect of its metallogenous
features is the Alpine geosyncline of the Maly Kavkaz situated between the Iran
and Kurin depression . In the Maly Kavkaz , similar structures and types of
deposits are ...
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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