Whole rock geochemistry of Forearc Basalts from IODP Expedition 352

doi:doi:10.1594/PANGAEA.895122

Whole rock geochemistry of Forearc Basalts from IODP Expedition 352

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.

BibTex:

@dataset{Shervais_John_W_and_Reagan_Mark_and_Haugen_Emily_and_Almeev_Renat_and_Pearce_Julian_and_Prytulak_Julie_and_Ryan_Jeffrey_G_and_Whattam_Scott_Andrew_and_Godard_Marguerite_and_Chapman_Timothy_and_Li_Hongyan_and_Kurz_Walter_and_Nelson_Wendy_R_and_Heaton_Daniel_and_Kirchenbaur_Maria_and_Shimizu_Kenji_and_Sakuyama_Tetsuya_and_Li_Yibing_and_Vetter_Scott_K_2018,
    abstract = {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.},
    author = {Shervais, John W and Reagan, Mark and Haugen, Emily and Almeev, Renat and Pearce, Julian and Prytulak, Julie and Ryan, Jeffrey G and Whattam, Scott Andrew and Godard, Marguerite and Chapman, Timothy and Li, Hongyan and Kurz, Walter and Nelson, Wendy R and Heaton, Daniel and Kirchenbaur, Maria and Shimizu, Kenji and Sakuyama, Tetsuya and Li, Yibing and Vetter, Scott K},
    doi = {10.1594/PANGAEA.895122},
    institution = {PANGAEA (Geophysics)},
    title = {Whole rock geochemistry of Forearc Basalts from IODP Expedition 352},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-895122},
    year = {2018}
}