Evolution of quartz cementation and burial history of the Eau Claire Formation based on in situ oxygen isotope analysis of quartz overgrowths

Individual quartz overgrowths in siltstone of the late Cambrian Eau Claire Formation (Fm.) are systematically zoned in oxygen isotope ratio (δ18O). In situ analysis of δ18O was performed with 3 and 15μm beam spots by secondary ion mass spectrometer (SIMS) on detrital quartz grains and quartz overgro...

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Veröffentlicht in:	Chemical geology 2014-09, Vol.384, p.168-180
Hauptverfasser:	Hyodo, Ayumi, Kozdon, Reinhard, Pollington, Anthony D., Valley, John W.
Format:	Artikel
Sprache:	eng
Schlagworte:	Basins Brines Cementation Eau Claire Formation Formations Illinois Basin Mathematical models Oxygen isotopes Quartz Quartz overgrowth Siltstone SIMS
Online-Zugang:	Volltext
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