Morphology, mode of formation, and diagenetic changes in framboids
Author(s) -
J. Kalliokoski,
L. M. Cathles
Publication year - 1969
Publication title -
bulletin of the geological society of finland
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.4
H-Index - 24
eISSN - 1799-4632
pISSN - 0367-5211
DOI - 10.17741/bgsf/41.014
Subject(s) - geology , diagenesis , morphology (biology) , paleontology , geochemistry
Pyrite framboids represent cubic close packed supermolecular colloid aggregates or »crystals», probably formed by a process of coacervation and particulation due to the reaction of ferruginous humic acid with biogenic H2S. The structures are enlarged and show morphological changes due to later diagenetic effects.
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