AbstractThe formation of pyrite (FeS2) from iron monosulfide precursors in
anoxic sediments has been suggested to proceed via mackinawite (FeS) and
greigite (Fe3S4). Despite decades of research, the mechanisms of pyrite
formation are not sufficiently understood because solid and dissolved
intermediates are oxygen-sensitive and poorly crystalline and therefore
notoriously difficult to characterize ... hiện toàn bộ
Yuxin Wu, Jonathan Ajo‐Franklin, Nicolas Spycher, Susan S. Hubbard, Guoxiang Zhang, Kenneth H. Williams, Joanna Taylor, Yoshiko Fujita, Robert W. Smith