Constraints and interpretation of 87Sr/86Sr ratios in Cenozoic dolomites

V. C. Vahrenkamp, P. K. Swart, Joaquin Ruiz

Research output: Contribution to journalArticle

17 Citations (Scopus)

Abstract

Replacement dolomitization by seawater has been modelled in order to quantify the Sr-isotope signature in Cenozoic dolomites. In a dolomitized core from Little Bahama Bank, Bahamas, two periods of dolomitization are recognized, one in the early Late Miocene involving Middle Miocene or older rocks, and a second one around 2.4 Ma ago affecting early Pliocene carbonates. -from Authors

Original languageEnglish (US)
Pages (from-to)385-388
Number of pages4
JournalGeophysical Research Letters
Volume15
Issue number4
StatePublished - 1988

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Bahamas
dolomitization
dolomite
Miocene
carbonates
Pliocene
isotopes
replacement
signatures
isotope
rocks
seawater
carbonate
rock

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

Constraints and interpretation of 87Sr/86Sr ratios in Cenozoic dolomites. / Vahrenkamp, V. C.; Swart, P. K.; Ruiz, Joaquin.

In: Geophysical Research Letters, Vol. 15, No. 4, 1988, p. 385-388.

Research output: Contribution to journalArticle

Vahrenkamp, V. C. ; Swart, P. K. ; Ruiz, Joaquin. / Constraints and interpretation of 87Sr/86Sr ratios in Cenozoic dolomites. In: Geophysical Research Letters. 1988 ; Vol. 15, No. 4. pp. 385-388.
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