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Missing western half of the Pacific Plate: Geochemical nature of the Izanagi-Pacific Ridge interaction with a stationary boundary between the Indian and Pacific mantles
The source mantle of the basaltic ocean crust on the western half of the Pacific Plate was examined using PbâNdâHf isotopes. The results showed that the subducted IzanagiâPacific Ridge (IPR) formed from both Pacific (180ââŒ80 Ma) and Indian (âŒ80â70 Ma) mantles. The western Pacific Plate becomes younger westward and is thought to have formed from the IPR. The ridge was subducted along the KurileâJapanâNankaiâRyukyu (KJNR) Trench at 60â55 Ma and leading edge of the Pacific Plate is currently stagnated in the mantle transition zone. Conversely, the entire eastern half of the Pacific Plate, formed from isotopically distinct Pacific mantle along the East Pacific Rise and the Juan de Fuca Ridge, largely remains on the seafloor. The subducted IPR is inaccessible; therefore, questions regarding which mantle might be responsible for the formation of the western half of the Pacific Plate remain controversial. Knowing the source of the IPR basalts provides insight into the IndianâPacific mantle boundary before the Cenozoic. Isotopic compositions of the basalts from borehole cores (165â130 Ma) in the western Pacific show that the surface oceanic crust is of Pacific mantle origin. However, the accreted ocean floor basalts (âŒ80â70 Ma) in the accretionary prism along the KJNR Trench have Indian mantle signatures. This indicates the younger western Pacific Plate of IPR origin formed partly from Indian mantle and that the IndianâPacific mantle boundary has been stationary in the western Pacific at least since the Cretaceous
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