Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Yoshio Nakasato"'
Publikováno v:
Earth, Planets and Space, Vol 70, Iss 1, Pp 1-10 (2018)
Abstract Hydrogenetic ferromanganese crusts (hereafter referred to as “crusts”) on Pacific seamounts are formed by the precipitation of iron–manganese oxides from seawater on volcanic and biogenic substrate rocks. As crusts grow continuously an
Externí odkaz:
https://doaj.org/article/dbe3575e16ce4dbf8723fbb39d285482
Publikováno v:
Earth, Planets and Space, Vol 70, Iss 1, Pp 1-10 (2018)
Hydrogenetic ferromanganese crusts (hereafter referred to as “crusts”) on Pacific seamounts are formed by the precipitation of iron–manganese oxides from seawater on volcanic and biogenic substrate rocks. As crusts grow continuously and have ve
Publikováno v:
Ore Geology Reviews. 87:62-70
Thick hydrogenetic ferromanganese (Fe Mn) crusts from the northwest and central Pacific seamounts often show a distinct dual structure composed of a typical hydrogenetic porous, friable upper part of Fe Mn oxides (Layer 1) and the underlying dense, h
Autor:
Teruhiko Kashiwabara, Katsuhiko Suzuki, Hisaaki Sato, Shingo Kato, Blair Thornton, Keisuke Nishi, Aya Sakaguchi, Shota Nitahara, Yoshio Nakasato, Koichi Iijima, Kyoko Yamaoka, Ayaka Tokumaru, Akira Usui, Tetsuro Urabe
Ferromanganese crusts cover all outcrops on Takuyo-Daigo seamount traversed during remotely operated underwater vehicle (ROV) dives, except in places covered by foraminifera sand. Takuyo-Daigo is a Cretaceous seamount located in the northwest Pacific
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4516d64591bbfd4990703c0b153c2b6a
https://eprints.soton.ac.uk/401146/
https://eprints.soton.ac.uk/401146/
Publikováno v:
Ore Geology Reviews. 86:980
Publikováno v:
Ore Geology Reviews. 86:981