Abstract
The combination of multiple sediment sources and varying rates of sediment accumulation in the Celebes and Sulu seas have had significant impact on the processes of diagenesis, mineralization, and pore-fluid flow. Isotopic and mass-balance calculations help elucidate the various reactions taking place in these western Pacific basins, where ash alteration and basalt-seawater interactions are superimposed on the effects of sulfate oxidation of organic carbon and biogenic methane and of dolomitization of biogenic carbonates. -from Authors
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CITATION STYLE
Von Breymann, M. T., Swart, P. K., Brass, G. W., & Berner, U. (1991). Pore-water chemistry of the Sulu and Celebes Seas: extensive diagenetic reactions at Sites 767 and 768. Proc., Scientific Results, ODP, Leg 124, Celebes and Sulu Seas, 203–215. https://doi.org/10.2973/odp.proc.sr.124.154.1991
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