Abstract
Chemical and mineralogical analyses were performed on samples from ten specially selected cores from the Red Sea geothermal deposit. The deposit was divided into seven bedded and laterally correlative facies as follows:
-
(1)
detrital
-
(2)
iron-montmorillonite
-
(3)
goethite-amorphous
-
(4)
sulfide
-
(5)
manganosiderite
-
(6)
anhydrite
-
(7)
manganite
Distribution of the facies, their unconsolidated nature and age relations indicate that the solids were precipitated out of the overlying brine column, that the area of brine discharge is very local within the Atlantis II Deep, and that the chemistry of the brine has changed considerably with time.
Mechanisms of precipitation include simple cooling of subterranean brine as it discharges into the bottom of the Atlantis II Deep and mixing of the brine with the overlying sea water.
Woods Hole Oceanographic Institution Contribution No. 2198.
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Bischoff, J.L. (1969). Red Sea Geothermal Brine Deposits: Their Mineralogy, Chemistry, and Genesis. In: Degens, E.T., Ross, D.A. (eds) Hot Brines and Recent Heavy Metal Deposits in the Red Sea. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-28603-6_37
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