Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating

Details Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating

Sep 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009jgre..11400b44g&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 73, iss. 21, p. 6488-6501.

Physics

4

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