Abstract
Onshore manganese nodules and vein coatings were recovered from Pliocene sedimentary beds in the Pisco Basin of southern Peru. Identified manganese minerals include todorokite and cryptomelane suggesting a diagenetic origin. However, the chemical composition suggests a mixed hydrogenetic/hydrothermal – diagenetic origin probably due to modification of the geochemical conditions caused by organic matter decay. The onshore exposition of Co-rich (up to 5,080 ppm) Mn nodules in the Pisco Formation suggests a possible novel economic potential to be confirmed by further study.
Original language | Spanish |
---|---|
Title of host publication | SGA2023 |
State | Published - 1 Jan 2023 |