作者: Martin Hartmann
DOI: 10.1007/978-3-662-28603-6_21
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摘要: Information is presented on the geochemistry of hot brines in Atlantis II Deep. Special emphasis given to origin manganese and iron source sulfur species both sediments brines. It concluded that fractionation principally a pH/Eh effect sulfate ions brine waters are derived from overlying Red Sea rather than supplied directly by discharging