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Seismic shear anisotropy in the lowermost mantle most likely results from elastic shear anisotropy and lattice preferred orientation of its constituent minerals, including perovskite, post-perovskite, and ferropericlase. Measurements of the elastic shear anisotropy of single-crystal (Mg0.9Fe0.1)O up to 69 gigapascals (GPa) show that it increased considerably across the pressure-induced spin transition of iron between 40 and 60 GPa. Increasing iron content further enhances the anisotropy. This leads to at least 50% stronger elastic shear anisotropy of (Mg,Fe)O in the lowermost mantle compared to MgO, which is typically used in geodynamic modeling. Our results imply that ferropericlase is the dominant cause of seismic shear anisotropy in the lower mantle.

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The predictive accuracy of STABLE-2000 and STABLE-2007 was examined within a prospective research design in a German-speaking sample of 263 adult male prison-released sexual offenders followed up for an average of 6.4 years. The STABLE-2007 was significantly related to all outcomes (AUC = 0.67-0.71), whereas the STABLE-2000 demonstrated only weak predictive accuracy for sexual reoffense (AUC = 0.62). Supporting the results of the construction sample, the STABLE-2007 incrementally added to the predictive accuracy of the STATIC-99 for violent and general reoffense (conviction and incarceration). Moreover, the STABLE-2007 total scores and the nominal risk/need categories made significant incremental contributions over the SORAG for predicting sexual reoffense.

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