Tectono‐magmatic processes investigated at deep‐water flanks of Hawaiian volcanoes
Jiro NakaEitarô TakahasiDavid A. ClagueM. O. GarciaTakeshi HanyuE. Herrero‐BerveraJ. IshibashiOsamu IshizukaK. JohnsonToshiya KanamatsuIchiro KaneokaPeter W. LipmanAlexander MalahoffGary M. McMurtryBrian P. MidsonJames G. MooreJulia K. MorganTakeshi NaganumaKatsuji NakajimaTamotsu OomoriA. J. PietruszkaKenji SatakeDavid R. SherrodTomo ShibataKen ShinozakiT. W. SissonJ.R. SmithS. TakaradaC. ThomberFrank A. TrusdellNohiro TsuboyamaT. UiSusumu UminoKozo UtoHisayoshi Yokose
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Abstract:
Hawaiian volcanoes are exceptional examples of intraplate hotspot volcanism. Hotspot volcanoes, which frequently host large eruptions and related earthquakes, flank‐failure landslides, and associated tsunamis, can present severe hazards to populated regions. Many studies have focused on subaerial parts of Hawaiian volcanoes, but the deep‐water flanks of the edifices, which can reach 5700 m below sea level, remain poorly understood because they are so inaccessible. In 1998 a collaborative program between Japan and the United States was initiated to explore the evolution of Hawaiian volcanoes, including their growth and degradation.Keywords:
Subaerial
Hotspot (geology)
Submarine volcano
Methodology, supplemental Figures S1–S11, and Tables S1 and S2.<br>
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EDITORIAL article Front. Earth Sci., 25 September 2023Sec. Volcanology Volume 11 - 2023 | https://doi.org/10.3389/feart.2023.1290315
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The scenic rim of southeastern Queensland, Australia: A history of mid Cenozoic intraplate volcanism
Intraplate volcanism was widespread in southeastern Queensland during the mid Cenozoic, leaving a legacy of variably eroded volcanoes and rugged topography known locally as The Scenic Rim. These plume-derived volcanoes provide a detailed record of northward Australian plate velocity, and indicate a major slowdown commencing at 26 Ma and persisting until 23 Ma, correlated with initial collision of the massive Ontong Java plateau with the northern subduction margin of the Australian plate. Despite traversing over 36 km of continental crust, trace element and isotopic signatures indicate little or only minor contamination for most units, with the exception of rhyolites formed during the period of slow plate velocity. Nevertheless, the thick continental crust allowed magmas to stall and fractionate during ascent, often producing highly evolved rocks (e.g., comendites) containing extreme concentrations of incompatible elements, including >2000 ppm Zr. Meanwhile, isotopic and trace element results from mafic units are consistent with melting and mixing of depleted upper mantle and an EM1-like source. Alkaline mafic eruptions also often contain abundant upper mantle and lower crustal xenoliths, providing excellent samples of these otherwise inaccessible regions. Denudation has produced good exposures of the subsurface magmatic architecture, a variety of landscapes, and diverse wildlife habitats; as a result many of the volcanoes are contained in National Parks, including the World Heritage listed Gondwana Rainforests of Australia.
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