K isotopes as a tracer of seafloor hydrothermal alteration
نویسندگان
چکیده
منابع مشابه
Hydrothermal sediment alteration at a seafloor vent field: Grimsey Graben, Tjörnes Fracture Zone, north of Iceland
[1] An active seafloor hydrothermal system subjects the background sediments of the Grimsey Graben (Tjörnes Fracture Zone) to alteration that produces dissolution of the primary volcaniclastic matrix and replacement/precipitation of sulfides, sulfates, oxides, oxyhydroxides, carbonates and phyllosilicates. Three types of hydrothermal alteration of the sediment are defined on the basis of the do...
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Article history: In situ sensors capable of re Received 8 August 2008 Received in revised form 8 November 2008 Accepted 10 November 2008 Available online xxxx Editor: R.L. Rudnick
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ژورنال
عنوان ژورنال: Proceedings of the National Academy of Sciences
سال: 2017
ISSN: 0027-8424,1091-6490
DOI: 10.1073/pnas.1609228114