The F'derik-Zouerate iron district: Mesoarchean and Paleoproterozoic iron formation of the Tiris Complex, Islamic Republic of Mauritania

Cliff D. Taylor; Carol A. Finn; Eric D. Anderson; Dwight Bradley; Mohamed Joud; Ahmed Taleb Mohamed; John D. Horton; Craig A. Johnson

doi:10.1007/978-3-319-31733-5

USGS · 70159535

The F'derik-Zouerate iron district: Mesoarchean and Paleoproterozoic iron formation of the Tiris Complex, Islamic Republic of Mauritania

Cliff D. Taylor·Carol A. Finn·Eric D. Anderson·Dwight Bradley·Mohamed Joud·Ahmed Taleb Mohamed·John D. Horton·Craig A. Johnson

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Abstract

High-grade hematitic iron ores (of HIF, containing 60-65 wt%Fe) have been mined in Mauritania since 1952 from Superior-type iron deposits of the F'derik-Zouerate district. Depletion of the high-grade ores in recent years has resulted in new exploration projects focused on lower-grade magnetite ores occurring in Algoma-type banded iron formation (of BIF, containing ca. 35 wt% Fe). Mauritania is the seventeenth largest iron producer in the world and currently has about 1.1 Gt of crude iron ore reserves.

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Cliff D. Taylor, Carol A. Finn, Eric D. Anderson, Dwight Bradley, Mohamed Joud, Ahmed Taleb Mohamed, John D. Horton, Craig A. Johnson. 2016. The F'derik-Zouerate iron district: Mesoarchean and Paleoproterozoic iron formation of the Tiris Complex, Islamic Republic of Mauritania. https://doi.org/10.1007/978-3-319-31733-5

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