The
REPt
2Al
3 compounds of the late rare-earth metals (
RE = Y, Dy–Tm) were found to crystallize isostructural. Single-crystal X-ray investigations of YPt
2Al
3 revealed an orthorhombic unit cell (
a = 1080.73(6),
b = 1871.96(9),
c = 413.04(2) pm,
wR2 = 0.0780, 942 F
2 values, 46 variables) with space group
Cmmm (
oC48;
q2pji2hedb). A comparison with the Pearson database indicated that YPt
2Al
3 forms a new structure type, in which the Pt and Al atoms form a [Pt
2Al
3]
δ− polyanion and the Y atoms reside in the cavities within the framework. Via a group-subgroup scheme, the relationship between the PrNi
2Al
3-type structure and the new YPt
2Al
3-type structure was illustrated. The compounds with
RE = Dy–Tm were characterized by powder X-ray diffraction experiments. While YPt
2Al
3 is a
Pauli-paramagnet, the other
REPt
2Al
3 (
RE = Dy–Tm) compounds exhibit paramagnetic behavior, which is in line with the rare-earth atoms being in the trivalent oxidation state. DyPt
2Al
3 and TmPt
2Al
3 exhibit ferromagnetic ordering at
TC = 10.8(1) and 4.7(1) K and HoPt
2Al
3 antiferromagnetic ordering at
TN = 5.5(1) K, respectively. Attempts to synthesize the isostructural lutetium compound resulted in the formation of Lu
2Pt
3Al
4 (Ce
2Ir
3Sb
4-type,
Pnma,
a = 1343.4(2),
b = 416.41(8),
c = 1141.1(2) pm), which could also be realized with thulium. The structure was refined from single-crystal data (
wR2 = 0.0940, 1605 F
2 values, 56 variables). Again, a polyanion with bonding Pt–Al interactions was found, and the two distinct Lu atoms were residing in the cavities of the [Pt
3Al
4]
δ– framework. X-ray photoelectron spectroscopy (XPS) measurements were conducted to examine the electron transfer from the rare-earth atoms onto the polyanionic framework.
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