“…The diffraction peaks of dolomite were found at 2θ = 31.04°, 41.22°, 45.01°, and 50.62°. Furthermore, the characteristic peaks of quartz were observed at 2θ = 20.84°, 26.63°, 42.48°, 50.13°, and 59.98° [23,31,32,33]. The typical diffraction peaks of Kal ( 2θ = 12.32° and 24.88°), Mt ( 2θ = 6.32°), Hal ( 2θ = 12.04° and 24.72°) and Sep ( 2θ = 7.39°) were all observed in their XRD patterns [31,34,35,36,37].…”