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The
X-ray diffraction is the ideal analysis method to obtain informations
about
crystalline
materials
structures
with
an atomic scale
and, as in our case, in minerals and rocks. In
particular, the powder diffraction allows to perform qualitative and
quantitative analysis of the mineralogical
composition of the material investigated.
  Rigaku diffractometer and diffractogram. From the diffractogram obtained we can acquire the following informations:
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