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Paleoclimate change reflected by element ratios of terrigenous sediments from deep-sea oxygen isotope MIS6 to MIS5 at MD12-3432 station in northern South China Sea
QU Huaxiang,HUANG Baoqi
Earth Science Frontiers . 2019, (
3
): 236 -242 . DOI: 10.13745/j.esf.sf.2019.4.18