Fig. 4From: Rock magnetic characterization of ferrimagnetic iron sulfides in gas hydrate-bearing marine sediments at Site C0008, Nankai Trough, Pacific Ocean, off-coast JapanSIRM evolution at low temperature (<300 K) for the three types of samples identified in Hole C0008A. Note the very well developed Verwey transition (magnetite) for the type 2 and the Besnus transition (pyrrhotite) for some type 3 samples. See text for discussionBack to article page