TY - JOUR
T1 - Marine 87Sr/86Sr ratios from the Jurassic to Pleistocene
T2 - evidence from groundwaters in Israel
AU - Starinsky, A.
AU - Bielski, M.
AU - Lazar, B.
AU - Wakshal, E.
AU - Steinitz, G.
PY - 1980/3
Y1 - 1980/3
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=0011337743&partnerID=8YFLogxK
U2 - 10.1016/0012-821X(80)90105-3
DO - 10.1016/0012-821X(80)90105-3
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AN - SCOPUS:0011337743
SN - 0012-821X
VL - 47
SP - 75
EP - 80
JO - Earth and Planetary Science Letters
JF - Earth and Planetary Science Letters
IS - 1
ER -