Use of strontium isotopes to constrain the timing and mode of dolomitization of upper Cenozoic sediments in a core from San Salvador, Bahamas

Geology
By: , and 

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Abstract

The 87Sr/86Sr ratios and the activity ratios of 234U/238U and 230Th/238U have been measured in dolomites from a 168-m-deep core taken on the island of San Salvador, Bahamas. These data suggest two periods of dolomitization. The first episode dolomitized Miocene age sediments during the latest Miocene, and the second dolomitized the Pliocene portion of the core and was still active as recently as 150 ka. The late timing of the second episode argues against penecontemporaneous models of dolomitization for the Pliocene sediments. Instead, dolomitization is favored either as a result of mixing-zone development during the large Pleistocene sea-level changes or by movement of seawater through the platform.

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Publication type Article
Publication Subtype Journal Article
Title Use of strontium isotopes to constrain the timing and mode of dolomitization of upper Cenozoic sediments in a core from San Salvador, Bahamas
Series title Geology
DOI 10.1130/0091-7613(1987)15<262:UOSITC>2.0.CO;2
Volume 15
Issue 3
Year Published 1985
Language English
Publisher Geological Society of America
Contributing office(s) Coastal and Marine Geology Program
Description 4 p.
First page 262
Last page 265
Country Bahamas
Other Geospatial San Salvador Island
Online Only (Y/N) N
Additional Online Files (Y/N) N
Google Analytic Metrics Metrics page
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