The use of particle-induced x-ray emission (PIXE) in conjunction with a sca
nning nuclear microprobe (SNM) offers one of the few microanalytical techni
ques capable of studies of elemental concentrations at the ppm level, with
a spatial resolution of the order of 1 mum. Beam scanning capabilities and
advanced data treatment make it a technique of choice for quantitative two-
dimensional studies of elemental distribution. Although the ultimate aim is
to obtain true quantitative elemental maps, free of concentration or thick
ness artifacts, some compromises are necessary owing to experimental and co
mputational restrictions. Some approaches currently used are discussed with
emphasis on true elemental imaging using the dynamic analysis method. Exam
ples of applications in geology and biology are shown to illustrate its ben
efits and limitations. Copyright (C) 2001 John Wiley & Sons, Ltd.