“… In the case of cordierite, from the same figure, diffraction peaks can be observed at 10.8, 18.3, 19.2, 21.9, 26.6, 28.7, 29.6, and 34.1° referred to 10 hkl miller planes of cordierite corresponded to (100), (110), (002), (102), (112), (202), (211), and (212), respectively, which are assigned to α-cordierite (JCPDS card no. 84–1222) . In the MIL-101 (Cr) case, the diffraction patterns primarily show characteristic peaks of two phases between 5 and 10°, typical for MIL-101 (Cr), and other characteristic diffraction peaks between 17 and 35°, which are typical for the presence of terephthalic acid .…”