Arculus, RJ and Ishizuka, O and Bogus, KA and Gurnis, M and Hickey-Vargas, R and Aljahdali, MH and Bandini-Maeder, AN and Barth, AP and Brandl, PA and Drab, L and do Monte Guerra, R and Hamada, M and Jiang, F and Kanayama, K and Kender, S and Kusano, Y and Li, H and Loudin, LC and Maffione, M and Marsaglia, KM and McCarthy, A and Meffre, S and Morris, A and Neuhaus, M and Savov, IP and Sena, C and Tepley III, FJ and van der Land, C and Yogodzinski, GM and Zhang, Z, Reply to Unclear causes for subduction', Nature Geoscience, 9, (5) pp. 338-339. ISSN 1752-0894 (2016) [Letter or Note in Journal]
Keenan and Encarnación suggest that the absence of pre-subduction inception basement in the drill core data taken from site U1438 raises ambiguity in our conclusion of spontaneous subduction initiation in the Izu–Bonin–Mariana system1. However, there is no evidence for uplift in the earliest products of the Izu–Bonin–Mariana system preceding rifting preserved anywhere in the region. Three sub-parallel ridges — from north to south, the Amami plateau, Daito and Oki-Daito ridges (Fig. 1 from ref. 1) — comprise magmatic products of Mesozoic–Tertiary arcs formed prior to the Izu–Bonin–Mariana system. These ridges generally strike east–west orthogonally to the Kyushu–Palau ridge — the earliest stratovolcano chain of the Izu–Bonin–Mariana system. If compression preceded inception, as implied by the forced subduction model2, we anticipate uplift of the old arc ridges, diminishing in effect westwards, and sediment shedding from uplifted regions into adjacent basins.
None of these predicted effects are observed. The Amami plateau, Daito and Oki-Daito ridges do not shallow eastwards, rather they shallow westwards3, possibly due to subsidence of the eastern sectors following inception of the Izu–Bonin–Mariana system4. Crustal thicknesses change rapidly across-strike of the ridges, showing no east–west compressional thickening3,4. Furthermore, Lower Eocene sedimentary sequences in the Minami Daito basin, which predate Izu–Bonin–Mariana inception, are clast-free mudstone5. Basalt sills intercalated with these sediments are alkaline intraplate types lacking subduction zone input, consistent with a rifting environment6. This lack of evidence for compression of pre-Izu–Bonin–Mariana basement, coupled with the rifting and seafloor spreading accompanying the earliest arc products that we document1 is consistent with a spontaneous initiation model.
Both forced and spontaneous subduction inception models2 are oversimplified. The process is likely to be strongly three-dimensional and probably propagates along-strike from an extant subduction system7. For the Izu–Bonin–Mariana system, northward propagation from a subduction zone on the southern boundary of the proto-Philippine Sea plate as the latter rotated clockwise is possible1. Juxtaposition of old, dense Pacific plate lithosphere against the relatively buoyant lithosphere of the Mesozoic to Lower Tertiary arcs could have been critical for the spontaneous nucleation of a new subduction zone8.
|Item Type:||Letter or Note in Journal|
|Keywords:||subduction initiation, Marianas, Izu, Bonin|
|Research Division:||Earth Sciences|
|Research Field:||Structural geology and tectonics|
|Objective Division:||Expanding Knowledge|
|Objective Group:||Expanding knowledge|
|Objective Field:||Expanding knowledge in the earth sciences|
|UTAS Author:||Meffre, S (Dr Sebastien Meffre)|
|Funding Support:||Australian Research Council (CE0561595)|
|Web of Science® Times Cited:||6|
|Deposited By:||CODES ARC|
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