



The ore bodies, although occurring in distinct re- gional belts (Eastern and Western Belt) are small and irregu- lar in size, shape and stratigraphy. After deposition the ores were overprinted by very low grade metamorphic events. Local geology The stratigraphic development of the Griqualand West Sequence in



The BIFs host a number of major high-grade iron ore deposits of Goa and Karnataka (Mukhopadhyay et al., 2008a). In the absence of a direct age from this succession a probable age bracket between 2.65 Ga and 2.5 Ga can be suggested for the Goa Group from the granitoids that are believed to be either part of the basement or …











The internal stratigraphy of the Marillana Creek palaeochannel Tertiary channel iron deposits (CID) in the Hamersley Province of Western Australia was initially defined in the 1980s and redefined as the Marillana Formation in the early 2000s. Recent drilling, open pit mining and field observations in the Western deposits at BHP Billiton Iron Ore's …



The stratigraphy of the Greenstone Belt in the Redcliff area originally mapped by McGregor (1937) and Tyndale-Biscoe (1949) has since been re-assessed, using ... The Ripple Creek iron ore deposit comprises the thickest portion of a long gossanous orebody that strikes northwest – southeast and forms a part of a 35km strike of gossanous











Survey, although the deposit was within a concession that had been granted to a prospecting company in 1910. By 1917 a company was formed to exploit the deposit, and production of direct-shipping ore began soon after, developing into one of the world's leading producers of the mid-1920s. Geological Setting



The iron ores are widespread in the Eastern and Western Deserts of Egypt. According to Egyptian Mineral Resource Authoriiy (EMRA 2015), there are nine known iron ore occurrences including Abu Marwat, Wadi Karim, Wadi El-Dabbah, Umm Ghamis El- Zarga, Gabal El-Hadid, Um-Nar, El Oweinat, Aswan, and Bahariya areas as illustrated in …



The Indian shield represents a vast repository of the Precambrian geological record. The Precambrian sedimentary basins were developed on four major Archaean nuclei (Dharwar, Bastar, Singhbhum and Aravalli–Bundelkhand; Fig. 1.1) and are comparable to those of Australia, South Africa, Canada and Brazil in scale and …



Map showing the location of Iron Ore Mines in India. Iron Ore mines are found in different regions of India. Iron Ore Distribution in India. India has significant reserves of iron ore, with the majority of the deposits located in the states of Odisha, Chhattisgarh, Jharkhand, Karnataka, and Goa. Iron ore resources are relatively …



Metallic ore deposits are anomalous accumulations of metal commodities within a few kilometres of the Earth's surface, which have been concentrated significantly above their average crustal contents and in mineralogical forms that make them economically and metallurgically exploitable (e.g., Skinner 1997).Although various …











The ~2.4 Ga Hotazel Formation of the Transvaal Supergroup of South Africa is best known for hosting the largest land-based manganese deposit in the world, namely the Kalahari Manganese Field. The Hotazel Formation comprises three sedimentary manganese ore beds interbedded with banded iron formation. Where the ~2.0 Ga pre-Gamagara …



The Kamoa copper deposit is located in the Katanga Province of the southern Democratic Republic of Congo outside of the area previously considered prospective for large copper deposits. With a 1% Cu cutoff, the hypogene ore zone of Kamoa spans over 81 km (super 2), varying in thickness from 2 to 15 m, and is currently laterally unconstrained.







The mining of stratiform ore deposits requires a means of determining the location of stratigraphic boundaries. A variety of geophysical logs may provide the required data but, in the case of banded iron formation hosted iron ore deposits in the Hamersley Ranges of Western Australia, only one geophysical log type (natural gamma) is collected for this …



DOI: 10.1016/j.cageo.2015.02.002 Corpus ID: 38276607; Automated recognition of stratigraphic marker shales from geophysical logs in iron ore deposits @article{Silversides2015AutomatedRO, title={Automated recognition of stratigraphic marker shales from geophysical logs in iron ore deposits}, author={Katherine L. …



The Palaeoproterozoic Transvaal Supergroup in the northern Cape Province of South Africa hosts high grade (>60 per cent Fe) hematitic and specularitic iron and manganese mineralisation. The mineralisation is primarily exposed along the western margin or in the central part of a major interference fold structure known as the Maremane dome. The …








