Li and Rau Reply: Bode et al., in a Comment [1] on our Letter [2], claim that the vortex (V) core width d vc in magnetic nanodisks (NDs) is on the order of 10 nm and essentially independent of the ND diameter d. We are presenting published data (see also Fig. 1) that clearly show that this claim is incorrect. For instance, a recent transmission electron microscopy experiment on d 6 m Co elements gives d vc 80 nm [3]. Their claim rests in a formula [Eq. (1) in Ref. [1] ] published by Feldtkeller and Thomas [4] for the Bloch line radius of thin films (d 1) with zero thickness D 0 and zero distance from the Bloch line center using Lilley's definition for the wall thickness [5]. We [6] and others [7] have already experimentally shown that the V wall thickness depends strongly on in patterned Co NDs. Equation (1) in Ref. [1] does not exhibit any dependence on d and D and should not be used for finite D and d. Usov and Peschany [8], Komineas [9], as well as Jubert and Allenspach [10]show that d vc depends on d and D. Data taken from Refs. [10,11] show that d vc changes at least by a factor of 4 with changing D (see Fig. 1). Buda et al. [11] remark that, increasing D, the out-of-plane demagnetization field decreases, and hence the exchange energy widens the V core. The failure of their claim can be more directly seen from Fig. 1, which gives d vc versus different d values obtained from recent publications [2 -19] together with a

Nyb6ite occurs as porphyroblasts in the Jianchang eclogite in the Donghai area, northeastern Jiangsu Province, eastern China. The Jianchang eclogite contains some inclusions of quartz after coesite in clinopyroxene, garnet and epidote. It has colourless to pale-violet pleochroism. A thin rim with violet pleochroism often develops around nyb6ite and is taramitic. It is further retrogressed by the symplectite which is mainly composed of hornblende, aegirine-augite and albite. Nyb6ite is associated with jadeitic pyroxene in the Jianchang eclogite, although other porphyroblastic amphiboles in other Donghai eclogites are barroisitic to katophoritic and are associated with omphacite.Fe-Mg partitioning between garnet and clinopyroxene and the presence of coesite pseudomorphs indicate P-T conditions in the Jianchang eclogite of about 740 + 60 ~ and more than 28 kbar. Similar P-T conditions were estimated for other porphyroblastic amphibole-bearing eclogites in the Donghai area. Nyb0ite can occur in the Na-A1-Fe-rich local bulk composition under the medium to high temperature and very high-pressure conditions. Retrograde rim amphibole is poorer in NaB, variable in Si content, and richer in Nan variable than the porphyroblastic amphibole in the Donghai area. This roughly implies a P-T path where P decreases without a large decrease of T.