Figure 2.
(a) Thomsen's anisotropy parameter |$\varepsilon $| vs. the content of clay minerals. (b) Thomsen's anisotropy parameter |$\gamma $| vs. the content of clay minerals.
(a) Thomsen's anisotropy parameter |$\varepsilon $| vs. the content of clay minerals. (b) Thomsen's anisotropy parameter |$\gamma $| vs. the content of clay minerals.
