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Retentivity of minerals for cosmogenic He and Ne

The extent to which Hcc is lost from quadz by diffusion was a matter of debate in the early nineties (e.g.. Ceding 1990 Graf et al. 1991 Trull et al. 1991 Brook and Kurz [Pg.763]

Discrimination of cosmogenic against trapped, radiogenic, and nucleogenic components [Pg.763]

To allow for an accurate determination of the concentration of a cosmogenic noble gas isotope, noble gas components from other sources must be effectively discriminated against. These components include  [Pg.763]

On the other hand, care must be taken to avoid irreversible adsorption of atmospheric noble gases on fresh grain surfaces (e.g., Niedermann and Eugster 1992), which may not be a problem for Ne in quartz but might affect certain other minerals. [Pg.764]

Nucleogenic He produced by the reaction Li(n,a) H(P ) He is only important in minerals with high Li content. The He/ He ratio resulting from U/Th decay and Li neutron capture can be estimated from the chemical composition of the mineral and [Pg.764]


See other pages where Retentivity of minerals for cosmogenic He and Ne is mentioned: [Pg.758]    [Pg.762]   


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And retention

Cosmogenic

Retention of

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