Marine 87Sr/86Sr ratios from the Jurassic to Pleistocene: evidence from groundwaters in Israel

Details Marine 87Sr/86Sr ratios from the Jurassic to Pleistocene: evidence from groundwaters in Israel Marine 87Sr/86Sr ratios from the Jurassic to Pleistocene: evidence from groundwaters in Israel

Mar 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980e%26psl..47...75s&link_type=abstract

Earth and Planetary Science Letters, Volume 47, Issue 1, p. 75-80.

Physics

3

Scientific paper

Oceanic 87Sr/86Sr ratios during Jurassic to Pleistocene have been determined by analysing fresh waters from marine limestone and dolomite aquifers. The results are in good agreement with published data from well preserved fossil material. The 87Sr/86Sr ratios obtained are 0.7070 for Lower to Middle Jurassic, 0.7075 for Late Cretaceous, 0.7080 for Lower to Middle Eocene and 0.7087 for Pleistocene aquifer waters. The value of 87Sr/86Sr for the Eimer and Amend isotopic standard was 0.7082.

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