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Why has the ocean mass been nearly constant ?: The role of deep mantle partial melting
Shun-ichiro KARATO
itemdescription
TitleWhy has the ocean mass been nearly constant ?: The role of deep mantle partial melting
AuthorsShun-ichiro KARATO
Data nameChikyukagaku (Geochemistry)
Volume56
Num4
Page99-108
Year2022
PublisherThe Geochemical Society of Japan
LanguageJA
Abstract languageEN
ISSN03864073
GEOLIS URLhttps://darc.gsj.jp/archives/detail?cls=geolis&pkey=300026155
DOI10.14934/chikyukagaku.56.99
@idhttps://gbank.gsj.jp/ld/resource/geolis/300026155