The Role of Iron and Mg/Ca Ratio in Dolomite Synthesis at 192°C

The reaction path that dolomite follows in its formation, approach to stoichiometry, and approach to order differs in the presence or absence of iron. Dolomite was synthesized in hydrothermal bombs using eight starter combinations heated at 192°C for eight time periods. When iron was present dolomit...

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Veröffentlicht in:	The Journal of geology 1995-01, Vol.103 (1), p.51-61
Hauptverfasser:	Lumsden, David N., Morrison, James W., Lloyd, Roger V.
Format:	Artikel
Sprache:	eng
Schlagworte:	Calcite Calcium Carbonates Crystals Dolomite Geology Iron mining Iron oxides Minerals Stoichiometry
Online-Zugang:	Volltext
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