149 Economic Geology
Tuesday, 30 October 2007
1:30 PM - 5:30 PM
GENESIS OF HIGH-GRADE IRON ORES OF THE ARCHEAN IRON ORE GROUP AROUND NOAMUNDI, INDIA
Paper number: 149-7
Program: Technical Sessions
Time: 2:35 PM – 2:50 PM
Authors
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Jens GutzmerTU Bergakademie, Freiberg, N/A
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Joydip MukhopadhyayPresidency College, Kolkata, N/A
Abstract
Hard hematite-martite ores formed by hydrothermal replacement of banded iron-formation protolith, not only through leaching of silica, but also introduction of iron by hydrothermal fluids of meteoric origin. The hydrothermal fluids evolved from one that was warm, acidic and reducing, to allow for transport of ferrous iron to one that was cooler and more alkaline to allow for dissolution of silica and precipitation of ferric iron, i.e. hematite and martite. Hematite iron ore pebbles in an overlying Mesoproterozoic conglomerate attest to the antiquity of the hard ores.
In Cretaceous-Cenozoic times leaching of silica and/or carbonate from partly mineralized banded iron-formation gave rise to formation of soft saprolitic ores. Weathering took place under the influence of highly reducing and acidic meteoric water, which is typical for lateritic soil profiles developed under humid tropical climatic conditions with lush plant cover..