Abstract
Concentration ratios of salinity to chlorinity and to sodium in interstitial waters are similar to those of Orca Basin bottom water, suggesting that the chemistry of interstitial water is affected by the dissolution of buried salt. -from Authors
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CITATION STYLE
APA
Ishizuka, T., Kawahata, H., & Aoki, S. (1986). Interstitial water geochemistry and clay mineralogy of the Mississippi Fan and Orca and Pigmy basins, Deep Sea Drilling Project Leg 96. Initial Reports DSDP, Leg 96, Ft. Lauderdale to Galveston, Texas, 1983, 711–728. https://doi.org/10.2973/dsdp.proc.96.142.1986
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