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Pyrite Formation in Organic‐rich Clay, Calcitic and Coal‐Forming Environments
Author(s) -
DEVIĆ Gordana,
PFENDT Petar,
JOVANĈIĆEVIĆ Branimir,
POPOVIC Zoran
Publication year - 2006
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/j.1755-6724.2006.tb00278.x
Subject(s) - pyrite , diagenesis , illite , organic matter , clay minerals , sedimentary rock , environmental chemistry , mineralogy , oxidizing agent , geology , sulfur , coal , chemistry , sediment , geochemistry , organic chemistry , geomorphology
The early diagenetic characteristics of pyrite formation processes in a Miocene freshwater sequence of mixed sediments (coal fragments in clays, sandstones or shales) alternating with continuous brown coal layers was investigated. Based on abundant minerals, the following main sedimentary environments were distinguished: the illite‐montmorillonitic (I‐M), calcitic (Ct) and coal‐forming environment (CL). For these hydrogeochemically differing environments the effects of limiting factors on the pyrite formation process (availability of sulphate and Fe, amount of organic matter and participation of organic sulphur) were assessed by correlation analysis. Significant differences in the effects of these limiting factors in the particular environments were observed. These differences were explained taking in account the different oxidative activity, Fe‐complex and surface complex forming properties of humic substances in dependence of pH of environment and the abundance of sorptionally active clay minerals. In environments having a relatively low pH and containing clay minerals (I‐M‐and CL‐environments) the oxidative activity of humic substances (Hs) on pyrite precursors was greatly prevented however pyrite formation depended on reactive Fe availability as the consequence of complex formation. On the contrary, in environments with a relatively high pH, as it was the calcitic, the oxidative activity of Hs was greatly enhanced, thus oxidizing the sulfur precursors of pyrite. The oxidation degree of organic matter was probably also a consequence of the differing activity of the humic electron‐acceptors.