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Alluvial fans in Buena Vista Valley, north-central Nevada, formed during at least four time periods during the late Quaternary as evidenced by four temporally and spatially constrained fan deposits: Qf1, Qf2, Qf3, and Qf4, from oldest to youngest. The stratigraphic relation between Qf3 and remnant beach ridge deposits of pluvial Lake Lahontan, the latter of which forms a paleoclimatic proxy for this...
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