作者: J. S. Turner
DOI: 10.1007/978-3-662-28603-6_18
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摘要: The observed temperature structure of the Red Sea brines, which occur as well-mixed layers separated by sharp interfaces, is compared with other natural examples layering and also laboratory experiments designed to study phenomenon. existence such characteristic liquids are stabilized salt but made unstable heating from below. Various possible mechanisms for their formation maintenance evaluated a physical point view. available evidence supports idea that source brines in Atlantis II Deep, overflowed into holes recent times.