The Norfolk Ridge: A Proximal Record of the Tonga‐Kermadec Subduction Initiation

Type Article
Date 2023-03
Language English
Author(s) Collot JORCID1, Sutherland R.ORCID2, Etienne S.ORCID1, Patriat MartinORCID3, Roest WalterORCID3, Marcaillou B.ORCID4, Clerc C.ORCID5, Stratford W.ORCID6, Mortimer N.ORCID6, Juan C.1, Bordenave A.ORCID1, Schnurle PhilippeORCID3, Barker D.ORCID6, Williams S.ORCID7, Wolf S.8, Crundwell M.ORCID6
Affiliation(s) 1 : Service Géologique de Nouvelle‐Calédonie (New Caledonia Geological Survey) DIMENC, Nouméa,New Caledonia
2 : Victoria University of Wellington, Wellington, New Zealand
3 : Université de Brest CNRS Ifremer Geo‐Ocean, Plouzané,France
4 : Université Côte d'Azur IRD CNRS Observatoire de la Côte d'Azur Valbonne, France
5 : Avignon université UMR 1114 EMMAH, Avignon,France
6 : GNS Science, Lower Hutt,New Zealand
7 : State Key Laboratory of Continental Dynamics Department of Geology Northwest University, Xían,China
8 : Sorbonne Université CNRS‐INSU Institut des Sciences de la Terre Paris ISTeP UMR 7193, Paris ,France
Source Geochemistry Geophysics Geosystems (1525-2027) (American Geophysical Union (AGU)), 2023-03 , Vol. 24 , N. 3 , P. e2022GC010721 (23p.)
DOI 10.1029/2022GC010721
WOS© Times Cited 1

Norfolk Ridge bounds the northeastern edge of the continent of Zealandia and is proximal to where Cenozoic Tonga-Kermadec subduction initiation occurred. We present and analyze new seismic reflection, bathymetric and rock data from Norfolk Ridge that show it is composed of a thick sedimentary succession and that it was formed and acquired its present-day ridge physiography and architecture during Eocene to Oligocene uplift, emergence and erosion. Contemporaneous subsidence of the adjacent New Caledonia Trough shaped the western slope of Norfolk Ridge and was accompanied by volcanism. Neogene extension along the eastern slope of Norfolk Ridge led to the opening of the Norfolk Basin. Our observations reveal little or no contractional deformation, in contrast to observations elsewhere in Zealandia, and are hence significant for understanding the mechanics of subduction initiation. We suggest that subduction nucleated north of Norfolk Ridge and propagated rapidly along the ridge during the period 40-35 Ma, giving it a linear and narrow shape. Slab roll-back following subduction initiation may have preserved the ridge and created its eastern flank. Our observations suggest that pre-existing structures, which were likely inherited from Cretaceous Gondwana subduction, were well-oriented to propagate rupture and create self-sustaining subduction.

Key Points

We present new marine geophysical and geological data of Norfolk Ridge located along the northeastern edge of the Zealandia continent

We show that the ridge is not inherited from Cretaceous rifting that led to isolation of Zealandia but from the TECTA Cenozoic tectonic event

Analysis of the structure and evolution of Norfolk Ridge underpins our understanding of tectonic processes of subduction initiation

Plain Language Summary

Plate tectonic theory established and proved that the surface of Earth is composed of rigid moving plates, but it remains unclear how and why these plates sometimes re-configure their boundaries and motions. Subduction zones are places where two plates converge and one plunges deep into the Earth beneath the other one. As the plate sinks, it drags the rest of the plate with it and acts as an engine that “pulls” the plate and drives horizontal motion. This is what drives the dynamics of plate tectonics. How are subduction zones created? This remains an open question, but we know from geological observations that new subduction zones do get created: more than half of all active subduction zones were created after the dinosaurs died out 65 million years ago. We present new observations from northern Zealandia (a submerged continent between New Zealand and New Caledonia) that document how one of the largest subduction zones on Earth, the Tonga-Kermadec system, started.

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Collot J, Sutherland R., Etienne S., Patriat Martin, Roest Walter, Marcaillou B., Clerc C., Stratford W., Mortimer N., Juan C., Bordenave A., Schnurle Philippe, Barker D., Williams S., Wolf S., Crundwell M. (2023). The Norfolk Ridge: A Proximal Record of the Tonga‐Kermadec Subduction Initiation. Geochemistry Geophysics Geosystems, 24(3), e2022GC010721 (23p.). Publisher's official version : , Open Access version :