Nick Mortimer M. Patriat Rose E. Turnbull M.P. Crundwell A. Agranier Andrew T. Calvert G. Seward Samuel Etienne P.M.J. Durance H.J. Campbell Julien Collot Phillip B. Gans 2023 <p><span>The 2015 VESPA voyage (Volcanic Evolution of South Pacific Arcs) was a seismic and rock dredging expedition to the Loyalty and Three Kings Ridges and South Fiji Basin. In this paper we present 33&nbsp;</span>⁴⁰<span>Ar/</span>³⁹<span>Ar, 22 micropaleontological, and two U/Pb ages for igneous and sedimentary rocks from 33 dredge sites in this little-studied part of the southwest Pacific Ocean. Igneous rocks include basalts, dolerites, basaltic andesites, trachyandesites, and a granite. Successful Ar/Ar dating of altered and/or low-K basalts was achieved through careful sample selection and processing, detailed petrographic and element mapping of groundmass, and incremental heating experiments on both phenocryst and groundmass separates to interpret the complex spectra produced by samples having multiple K reservoirs. The&nbsp;</span>⁴⁰<span>Ar/</span>³⁹<span>Ar ages of most of the sampled lavas, irrespective of composition, are latest Oligocene to earliest Miocene (25–22&nbsp;Ma); two are Eocene (39–36&nbsp;Ma). The granite has a U/Pb zircon age of 23.6&nbsp;±&nbsp;0.3&nbsp;Ma.&nbsp;</span>⁴⁰<span>Ar/</span>³⁹<span>Ar lava ages are corroborated by microfossil ages from associated sedimentary rocks. The VESPA lavas are part of a &gt;3,000&nbsp;km long disrupted belt of Eocene to Miocene subduction-related volcanic rocks. The belt includes arc rocks in Northland New Zealand, Northland Plateau, Three Kings Ridge, and Loyalty Ridge and, speculatively, D’Entrecasteaux Ridge. This belt is the product of superimposed Eocene and Oligocene-Miocene remnant volcanic arcs that were stranded along and near the edge of Zealandia while still-active arc belts migrated east with the Pacific trench.</span></p> application/pdf 10.1029/2022GC010670 en American Geophysical Union Detailed 40Ar/39Ar geochronology of the Loyalty and Three Kings Ridges clarifies the extent and sequential development of Eocene to Miocene southwest Pacific remnant volcanic arcs article