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Earth, Planets and Space
Fig. 5 | Earth, Planets and Space

Fig. 5

From: Rock magnetic characterization of ferrimagnetic iron sulfides in gas hydrate-bearing marine sediments at Site C0008, Nankai Trough, Pacific Ocean, off-coast Japan

Fig. 5

δFC versus δZFC diagram. δ = (M 80K–M 150K)/M 80K where M is the remanence at low temperature (Moskowitz et al. 1993). Note the distribution of the δ values according to the samples types (T1, T2 and T3). Data from Hole C0008A are from this study; data from Hole C0008C are from Kars and Kodama (2015) 1, 2, 3 and 4 on the 1:1 line refer respectively to the samples 17H-7-19-21, 15H-4-42-44, 13H-2-122.5-124.5 and 19H-1-142-144 shown on Fig. 4

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