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Page 8
One can distinguish here three ore belts , their borders coinciding with the
position of the main structural zones : ( a ) chromite ore belt confined to the axial
part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the ...
One can distinguish here three ore belts , their borders coinciding with the
position of the main structural zones : ( a ) chromite ore belt confined to the axial
part of the Baluchistan geosyncline , ( b ) mercury - antimony belt occupying the ...
Page 10
The first is due to the appearance of small chromite deposits in Ras Koh range ,
which are beyond the chromite ore belt , in the tectonic suture bordering the
Chagai median messifs in the south . The second exception is , that the fluorite ...
The first is due to the appearance of small chromite deposits in Ras Koh range ,
which are beyond the chromite ore belt , in the tectonic suture bordering the
Chagai median messifs in the south . The second exception is , that the fluorite ...
Page 12
Ore zones : 22 Chromite confined to fracture zones in the trough part of the
geosyncline ; 23 — Chromite in fracture zon on the jointing of geosynclinal
marginal troughs with median massifs ; 24 — Possible extension of Hinduba
chromite zone ...
Ore zones : 22 Chromite confined to fracture zones in the trough part of the
geosyncline ; 23 — Chromite in fracture zon on the jointing of geosynclinal
marginal troughs with median massifs ; 24 — Possible extension of Hinduba
chromite zone ...
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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