# Citation: Milaneschi, L.; Mattei, M.; Cornamusini, G.; Foresi, L. M.; Martini, I.; Cifelli, F. (2025): Anisotropy of Magnetic Susceptibility and Magnetic Mineralogy Dataset from the Neogene Valdelsa Basin (Southern Tuscany, Italy). GFZ Data Services. https://doi.org/10.5880/fidgeo.2025.028
# Licence: Creative Commons Attribution 4.0 International License (CC BY 4.0); https://creativecommons.org/licenses/by/4.0/
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ID            Specimen      Field         Frequency     Kmean         L             F             P             Pj            T             U             Q             E             Kmax_Dec      Kmax_Inc      Kint_Dec      Kint_Inc      Kmin_Dec      Kmin_Inc      FTest_F       FTest_F12     FTest_F23     E12           E23           E13           
1             VE0601        423           875           1.73710254850034E-04        1.001753      1.030185      1.031991      1.036027      0.8887567     0.8870949     5.809226E-02  1.028382      349.489395262475            17.6017071226402            257.414554900002            6.51043595932217            147.876931172586            71.1582039175056            0             0             0             0             0             0             
2             VE0602        423           875           1.9879234259984E-04         1.004179      1.03329       1.037608      1.041266      0.7740596     0.7703425     0.1218231     1.028989      327.795877625525            17.9802425452087            60.7715770357526            9.08794915774548            176.409555593266            69.7111947747842            0             0             0             0             0             0             
3             VE0603        423           875           1.95543765528867E-04        1.005647      1.023031      1.028808      1.030532      0.6034769     0.5989497     0.2228708     1.017287      356.884533790774            1.85937113955883            266.289480431242            17.7398901264348            92.6725684309925            72.1564493170438            0             0             0             0             0             0             
