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- W1505352832 abstract "Publisher Summary In biological and particularly bacterial activity, hydrothermalism, alteration of substrates, and early diagenetic processes interact to form hydrogenous sediments. As a result, hydrogenous sediments include a variety of components. Besides evaporates, hydrogenous components include hydrothermal deposits, metalliferous elements, such as polymetallic nodules and crusts, and a variety of authigenic minerals. This chapter focuses on metalliferous and authigenic deposits, which have not been described before and are either widespread in the ocean or characteristic of specific environmental conditions. They include polymetallic nodules and crusts, glauconite, and phosphates. First recovered from the deep ocean during the Challenger Expedition, polymetallic nodules are mainly concentrated on the seafloor of the deepest basins, whereas polymetallic crusts are principally associated to submarine volcanic systems and seamounts. Overall, there is a strong relationship between seawater and the geochemical composition of many metalliferous deposits. Although chemical elements of hydrothermal origin largely dominate, local environmental conditions may also play a role in the elemental content of metalliferous deposits. For example, polymetallic crusts and nodules may include elements of biogenic origin (Ba, Ca, P, etc.) or detrital origin (Si, Al, etc.)." @default.
- W1505352832 created "2016-06-24" @default.
- W1505352832 creator A5063960368 @default.
- W1505352832 date "2008-01-01" @default.
- W1505352832 modified "2023-10-05" @default.
- W1505352832 title "Chapter Thirteen Hydrogenous Sediments" @default.
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- W1505352832 doi "https://doi.org/10.1016/s1572-5480(08)00213-3" @default.
- W1505352832 hasPublicationYear "2008" @default.
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