“…5, 6 and 7 for MSA, AESA and OSA. MSA and AESA show almost the same appearance and reveal the existence of major peaks at 20° and 21° for MSA 14° and 18° for AESA of kaolinite and mica/illite, which correspond to the pattern of the amorphous nature (Bahoria et al 2018;Yin et al 2018), while OSA shows many peaks corresponding to the position 2 21°, 26°, 27°, 29°, 31°, 33°, 36°, 38°, 39°, 41°, 43°, 46°, 48°, 50° and 53°, respectively, whereas mica/illite predominate over quartz (Jiang et al 2018;Benafqir et al 2019). If the material under investigation is crystalline, well-defined peaks are observed, while non-crystalline or amorphous system shows a hollow instead of well-defined peaks (Hajji et al 2017;Zhao et al 2017).…”