Das bislang Pb-reichste bekannte Material wurde von Walenta beschrieben:
Walenta, K. (2003): Monokliner bleihaltiger Rhabdophan von der Grube Clara im mittleren Schwarzwald. Aufschluss 54, 405-409.
Plumbiferous rhabdophane occurs among the secondary minerals of the Clara Mine in the Central Black Forest, Germany, and is assocd. with quartz, pyromorphite, and limonite. It forms spherulitic aggregates on quartz composed of acicular crystals elongated [010] and reaching 0.05 mm in length. Color yellow, yellowish brown, or pale brown, translucent, streak white, luster silky, no cleavage obsd., fracture uneven. Hardness 3.5, d. (calc.) 4.49 g/cm3. Optical data: n 1.772(3), n 1.772(3), n 1.812(3), uniaxial or weakly biaxial (+), Z = b. Unit-cell dimensions a 7.04(1), b 6.42(1), c 7.22(1) .ANG., 120.00(10), Z = 3. Result of anal.: Y2O3 1.53, UO2 0.77, CaO 0.41, La2O3 9.70, Ce2O3 16.57, Nd2O3 10.24, Sm2O3 3.00, Al2O3 0.38, PbO 21.32, CuO 0.24, SiO2 0.13, P2O5 25.63, As2O5 0.14, H2O (by difference) 9.94, total 100.00%, yielding the formula (Ce0.26Pb0.24Nd0.16La0.15Sm0.04Y 0.03Ca0.02U0.01Cu0.01Al0.02) 0.94 (P0.92Si0.02)0.94H2.80O5 on the basis of 5 O atoms or simplified (REE,PbH)PO4.H2O.
Anmerkung: nach der dominant-constituent rule ist REE >> Pb, das Material kommt also nicht mal in die Nähe eines Pb-Endglieds.