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Strontium isotope constraints on fluid flow in the upper oceanic crust at the East Pacific Rise

✍ Scribed by Kathryn M. Gillis; Laurence A. Coogan; Rolf Pedersen

Book ID
116451885
Publisher
Elsevier Science
Year
2005
Tongue
English
Weight
284 KB
Volume
232
Category
Article
ISSN
0012-821X

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Strontium isotopic differences between the basalts from the East Pacific and the Chile Rises (0.7026-0.7035, average 0.7028) and abyssal hills (0.7025-0.7037, average 0.7033) suggest that these are produced from different source materials. A progressive increase of K/Rb with decrease in SIz~/Sr s6 r