Details
Zusammenfassung: <jats:p>The surficial sediments of Fayetteville Green Lake show laminated and unlaminated beds. Couplets of a basal pale and an overlying dark lamina are varves. Unlaminated beds are probably deposited from density currents. Varve sedimentation averages 0.07 g cm<jats:sc><jats:sup>−2</jats:sup></jats:sc> yr<jats:sup>−1</jats:sup> dry wt or 0.05 g cm<jats:sup>−2</jats:sup> yr<jats:sup>−1</jats:sup> CaCO<jats:sub>3</jats:sub>. Turbidites account for 40 to 65% total sediment accumulation.</jats:p>
Umfang: 848-857
ISSN: 0024-3590
1939-5590
DOI: 10.4319/lo.1969.14.6.0848