Abstract
Pore fluid chemistry in the upper meter of carbonate sediments from the Florida Keys (Florida Bay, Atlantic reef tract) reveals that carbonate dissolution is common and may be volumetrically significant. -from Authors
Cite
CITATION STYLE
APA
Walter, L. M., & Burton, E. A. (1990). Dissolution of recent platform carbonate sediments in marine pore fluids. American Journal of Science, 290(6), 601–643. https://doi.org/10.2475/ajs.290.6.601
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