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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

التفاصيل البيبلوغرافية
العنوان: 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
المؤلفون: P. B. Gans, N. Mortimer, M. Patriat, R. E. Turnbull, M. P. Crundwell, A. Agranier, A. T. Calvert, G. Seward, S. Etienne, P. M. J. Durance, H. J. Campbell, J. Collot
المصدر: Geochemistry, Geophysics, Geosystems, Vol 24, Iss 2, Pp n/a-n/a (2023)
بيانات النشر: Wiley, 2023.
سنة النشر: 2023
المجموعة: LCC:Geophysics. Cosmic physics
LCC:Geology
مصطلحات موضوعية: SW Pacific, tectonics, geochronology, subduction, volcanic arcs, Cenozoic, Geophysics. Cosmic physics, QC801-809, Geology, QE1-996.5
الوصف: Abstract 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 40Ar/39Ar, 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 40Ar/39Ar ages of most of the sampled lavas, irrespective of composition, are latest Oligocene to earliest Miocene (25–22 Ma); two are Eocene (39–36 Ma). The granite has a U/Pb zircon age of 23.6 ± 0.3 Ma. 40Ar/39Ar lava ages are corroborated by microfossil ages from associated sedimentary rocks. The VESPA lavas are part of a >3,000 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.
نوع الوثيقة: article
وصف الملف: electronic resource
اللغة: English
تدمد: 1525-2027
Relation: https://doaj.org/toc/1525-2027
DOI: 10.1029/2022GC010670
URL الوصول: https://doaj.org/article/2b5f939c99254d0e8e08d22bfbc5424f
رقم الأكسشن: edsdoj.2b5f939c99254d0e8e08d22bfbc5424f
قاعدة البيانات: Directory of Open Access Journals
الوصف
تدمد:15252027
DOI:10.1029/2022GC010670