Articles | Volume 15, issue 2
https://doi.org/10.5194/se-15-167-2024
https://doi.org/10.5194/se-15-167-2024
Research article
 | 
08 Feb 2024
Research article |  | 08 Feb 2024

Contribution of carbonatite and recycled oceanic crust to petit-spot lavas on the western Pacific Plate

Kazuto Mikuni, Naoto Hirano, Shiki Machida, Hirochika Sumino, Norikatsu Akizawa, Akihiro Tamura, Tomoaki Morishita, and Yasuhiro Kato

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Cited articles

Aftabuzzaman, M. R., Yomogoda, K., Suzuki, S., Takayanagi, H., Ishigaki, A., Machida, S., Asahara, Y., Yamamoto, K., Hirano, N., Sano, S.-I., Chiyonobu, S., Bassi, D., and Iryu, Y.: Multi-approach characterization of shallow-water carbonates off Minamitorishima and their depositional settings/history, Isl. Arc, 30, e12400, https://doi.org/10.1111/iar.12400, 2021. 
Akizawa, N., Ohara, Y., Okino, K., Ishizuka, O., Yamashita, H., Machida, S., Sanfilippo, A., Basch, V., Snow, J. E., Sen, A., Hirauchi, K.-I., Michibayashi, K., Harigane, Y., Fujii, M., Asanuma, H., and Hirata, T.: Geochemical characteristics of back-arc basin lower crust and upper mantle at final spreading stage of Shikoku Basin: an example of Mado Megamullion, Prog. Earth Planet. Sci., 8, 65, https://doi.org/10.1186/s40645-021-00454-3, 2021. 
Akizawa, N., Hirano, N., Matsuzaki, K. M., Machida, S., Tamura, C., Kaneko, J., Iwano, H., Danhara, T., and Hirata, T.: A direct evidence for disturbance of whole sediment layer in the subducting Pacific plate by petit-spot magma–water/sediment interaction, Mar. Geol., 444, 106712, https://doi.org/10.1016/j.margeo.2021.106712, 2022. 
Asimow, P. D. and Langmuir, C. H.: The importance of water to oceanic mantle melting regimes, Nature, 421, 815–820, https://doi.org/10.1038/nature01429, 2003. 
Audhkhasi, P. and Singh, S. C.: Discovery of distinct lithosphere-asthenosphere boundary and the Gutenberg discontinuity in the Atlantic Ocean, Sci. Adv., 8, eabn5404, https://doi.org/10.1126/sciadv.abn5404, 2022. 
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Short summary
Plate tectonics theory is the motion of rocky plates (lithosphere) over ductile zones (asthenosphere). The causes of the lithosphere–asthenosphere boundary (LAB) are controversial; however, petit-spot volcanism supports the presence of melt at the LAB. We conducted geochemistry, geochronology, and geochemical modeling of petit-spot volcanoes on the western Pacific Plate, and the results suggested that carbonatite melt and recycled oceanic crust induced the partial melting at the LAB.