The Argash antimony ore deposit is located at south of Neyshabour and the eastern part of the Sabzevar zone. This deposit occurs within a sequence of Eocene-Oligocene volcanic-intrusion rocks. The mineralization occurs as open space filling, taking place as irregular veins, veinlets and hydrothermal breccias. The mineralogy of the veins is comparatively simple. The primary antimony-bearing mine...

The ore bodies of Galali and Baba-Ali are two relatively important iron ore deposits in west Iran.  These ore deposits are situated in the Sanandaj-Sirjan zone. The deposits are associated with ultramafic, calc-alkaline, carbonatite and other rocks. Macroscopic observations, on the boreholes, show that one of the rare ultramafic rocks (hornblendite) appears in all various horizons parallel to m...

Geochemical variations of the Pro terozoic dolomite samples close to the ore deposits in the Renison mine area, Tasmania, Austra lia. arc the result of alteration. The oxygen tsotope va lues of the most altered dolomites surrounding the orc deposit indicates that these arc affected oy hot (up to abou t 350°C) hydro thermal nuids. There is a trend of decreasing lighter oxygen and carbon is...

To serve Indian economy railways carry different category of freight traffics like coal, iron ore, food grains, steel, fertilizer and mineral oil, etc. Dispersal of some of these freights is limited compared to other traffics which ambit of outreach is quite large. Food grains and fertilizers are such freights which reach wider section of population, transporting thereby railways carry off its ...