Journal
ORE GEOLOGY REVIEWS
Volume 63, Issue -, Pages 465-469Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.oregeorev.2014.03.009
Keywords
Algoma-type; Banded iron formations; Experimental simulation; Genetic mechanism; Precambrian
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Funding
- Major State Basic Research Development Program of China [2012CB416602]
- State Key Laboratory of Ore Deposit Geochemistry, Chinese Academy of Sciences [SKLODG-ZY125-01]
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A series of experimental simulations of the genetic mechanism of banded iron formations has been conducted using a suite of self-designed glassware to model the hypergene circulation of surface water. The simulation process involved two parts: in the first part, the weathering and leaching of basalt by strongly acidic meteoric water during early Precambrian volcanism would have resulted in amorphous silica precipitation and strongly acidic ore-bearing solutions (pH < 1.25). And in the second part, during quiescent volcanism, the weathering and leaching of basalt by CO2-saturated meteoric water without contamination of other volcanic gases would increase the pH value of the solution. When the pH increased to 1.25-5.50, ferric hydroxides and amorphous silica would alternately precipitate owing to periodic heating and continuous addition of high-pH basalt-leaching solutions. This is a possible explanation of the genetic mechanism of the Algoma-type banded iron formations. (C) 2014 Elsevier B.V. All rights reserved.
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