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Fig. 6 Representative X-ray diffraction patterns of Fe-Mn crust from western Pacific Magellan Seamount. Vernatide(V), Quartz(Q), Feldspar(F), Smectite(S) and Carbonate fluorapatite(CFA) were consisted in Fe-Mn crust.
Econ. Environ. Geol. 2023;56:55~63 https://doi.org/10.9719/EEG.2023.56.1.55
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