“…Upon sulfurization, PXRD analysis reveals that the obtained Sample-800 has lower crystallinity than that of precursor, but a broad diffraction peak at around 25° appears, which can be assigned to the characteristic (002) plane of the rGO sheets and the graphitic carbon derived from the MOF skeleton ( Figure 1c). [15] The peaks at 30.084°, 35.437°, 43.058°, 56.973°, and 62.585° correspond well to the (220), (311), (400), (511), and (440) planes of CoFe 2 O 4 (JCPDS: 22-1086), respectively. The others at 30.516°, 35.178°, 46.762° 54.266°, and 74.402° are indexed to the (100), (101), (102), (110), and (202) planes of Co 1−x S (JCPDS: 42-0826).…”