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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

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

Fig. 3

Low temperature rock magnetic experiment results of two samples from Site U1424. a Saturation isothermal remanent magnetization acquired at room temperature (RT-SIRM) monitored on cooling from 300 to 10 K and subsequent warming back to 300 K; b SIRM acquired at low temperature (LT-SIRM) after zero-field cooling monitored on warming; and c derivative of the LT-SIRM warming curves. Note that RT-SIRM and LT-SIRM curves have been normalized to SIRM of samples at 300 K and at 10 K respectively. The derivatives of LT-SIRM were calculated based on a smoothed version of the raw data to avoid influence from occasional noisy measurements. Depth of samples listed is in m CCSF-A

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