Whole rock geochemistry of Forearc Basalts from IODP Expedition 352
Fuente:
PANGAEA
Enregistré dans:
| Auteurs principaux: | , , , , , , , , , , , , , , , , , , |
|---|---|
| Format: | Dataset Open Access |
| Langue: | en |
| Publié: |
PANGAEA
2018
|
| Sujets: | |
| Accès en ligne: | |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
| _version_ | 1867171859444793344 |
|---|---|
| author | Shervais, John W Reagan, Mark Haugen, Emily Almeev, Renat Pearce, Julian Prytulak, Julie Ryan, Jeffrey G Whattam, Scott Andrew Godard, Marguerite Chapman, Timothy Li, Hongyan Kurz, Walter Nelson, Wendy R Heaton, Daniel Kirchenbaur, Maria Shimizu, Kenji Sakuyama, Tetsuya Li, Yibing Vetter, Scott K |
| author_facet | Shervais, John W Reagan, Mark Haugen, Emily Almeev, Renat Pearce, Julian Prytulak, Julie Ryan, Jeffrey G Whattam, Scott Andrew Godard, Marguerite Chapman, Timothy Li, Hongyan Kurz, Walter Nelson, Wendy R Heaton, Daniel Kirchenbaur, Maria Shimizu, Kenji Sakuyama, Tetsuya Li, Yibing Vetter, Scott K |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | These basalts represent the earliest response to subduction initiation in the Izu-Bonin arc system during the early Eocene. They are highly refractory and formed by high degrees of partial melting of a previously depleted source. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_895122 |
| institution | PANGAEA |
| language | en |
| publishDate | 2018 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Whole rock geochemistry of Forearc Basalts from IODP Expedition 352 Shervais, John W Reagan, Mark Haugen, Emily Almeev, Renat Pearce, Julian Prytulak, Julie Ryan, Jeffrey G Whattam, Scott Andrew Godard, Marguerite Chapman, Timothy Li, Hongyan Kurz, Walter Nelson, Wendy R Heaton, Daniel Kirchenbaur, Maria Shimizu, Kenji Sakuyama, Tetsuya Li, Yibing Vetter, Scott K 352-U1440A; 352-U1440B; 352-U1441A; Aluminium oxide; Barium; Calcium oxide; Calculated from weight loss after ignition at 450 °C; CDRILL; Cerium; Chromium; Cobalt; Core drilling; DEPTH, sediment/rock; Dysprosium; Erbium; Europium; Event label; Event layer type; Exp352; Gadolinium; Hafnium; Holmium; IBM; ICP-MS; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Iron oxide, Fe2O3; Iron oxide, FeO; Izu-Bonin-Mariana fore arc; Joides Resolution; Lanthanum; Lead; Loss on ignition; Lutetium; Magnesium oxide; Manganese oxide; Mass; Neodymium; Nickel; Niobium; Phosphorus pentoxide; Potassium; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Sample ID; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Terbium; Thorium; Thulium; Titanium; Titanium dioxide; Unit; Uranium; Vanadium; X-ray fluorescence (XRF); Ytterbium; Yttrium; Zirconium These basalts represent the earliest response to subduction initiation in the Izu-Bonin arc system during the early Eocene. They are highly refractory and formed by high degrees of partial melting of a previously depleted source. |
| title | Whole rock geochemistry of Forearc Basalts from IODP Expedition 352 |
| topic | 352-U1440A; 352-U1440B; 352-U1441A; Aluminium oxide; Barium; Calcium oxide; Calculated from weight loss after ignition at 450 °C; CDRILL; Cerium; Chromium; Cobalt; Core drilling; DEPTH, sediment/rock; Dysprosium; Erbium; Europium; Event label; Event layer type; Exp352; Gadolinium; Hafnium; Holmium; IBM; ICP-MS; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Iron oxide, Fe2O3; Iron oxide, FeO; Izu-Bonin-Mariana fore arc; Joides Resolution; Lanthanum; Lead; Loss on ignition; Lutetium; Magnesium oxide; Manganese oxide; Mass; Neodymium; Nickel; Niobium; Phosphorus pentoxide; Potassium; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Sample ID; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Terbium; Thorium; Thulium; Titanium; Titanium dioxide; Unit; Uranium; Vanadium; X-ray fluorescence (XRF); Ytterbium; Yttrium; Zirconium |
| url | https://doi.org/10.1594/PANGAEA.895122 |