95 7 dating
1b) is dominated by smectite with subordinate illite and kaolinite.
1a), but with dominant interstratified illite-smectite. In contrast, the saprolitic sample closest to the hosting fresh granodiorite (sample ‘Bømlo 2’ in Fig.
The following table shows all the Qumran-related samples that were tested by Zurich (Z), Tucson (T) and Libby (L).