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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Integrated Pliocene-Pleistocene magnetostratigraphy and tephrostratigraphy of deep-sea sediments at IODP Site U1424 (Yamato Basin, Japan Sea)

Fig. 2

Room temperature rock magnetic analyses results of selected bulk sediment samples from Site U1424. Measurements were conducted on a vibrating sample magnetometer (VSM). a Slope corrected hysteresis loops. b IRM backfield curves. c Hysteresis parameters plotted on a Day et al. (1977) plot. d IRM acquisition data. e Gradient of IRM acquisition. f, g FORC diagrams. Hysteresis loops, IRM backfield experiment, and IRM acquisition data are weight normalized. Gradient of IRM curves are normalized so that total area underneath each curve is equal to 1. Color of data curves and points in (b) and (c) share the same key shown in (a), and data curves in (e) share the same key shown in (d). Depth of samples listed is in m CCSF-A

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