验证Ontong Java Nui假说:地球上最大的超级火山

IF 0.2 Q4 GEOGRAPHY, PHYSICAL
T. Sano, M. Tejada, M. Nakanishi, T. Hanyu, S. Miura, D. Suetsugu, T. Tonegawa, A. Ishikawa, K. Shimizu, S. Shimizu
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引用次数: 4

摘要

大火成岩省(LIPs),如赤道西太平洋的Ontong爪哇高原(OJP),提供了地幔过程和组成的信息,它们的形成可能对全球环境产生影响。OJP是最大的海洋高原,可能是地球上体积最大的火成岩大厦。尽管它很重要,但OJP的大小、体积和形成速度还没有得到很好的限制。与OJP相关的火山活动的最大范围可能比目前估计的还要大,因为火山学研究表明,来自OJP的长熔岩流(或岩)可能已经到达邻近的瑙鲁、东马里亚纳和可能的皮加菲塔盆地。此外,来自Ontong爪哇、Hikurangi和Manihiki高原的熔岩在年龄和一些地球化学上的相似性表明,它们可能曾经是一个LIP (Ontong Java Nui, OJN)的一部分。如果这是真的,巨大的火山活动可能覆盖*国立科学博物館地学研究部* *海洋研究開発機構海域地震火山部門火山・地球内部研究センター* * *千葉大学大学院理学研究院* * * *海洋研究開発機構海域地震火山部門地震発生帯研究センター* * * * *東京工業大学地球惑星科学系* * * * * *海洋研究開発機構超先鋭研究開発部門高知コア研究所* * * * * * *千葉大学大学院融合理工学府*地质学和古生物学、国家自然博物馆和科学,筑波,305 - 0005年,日本* *火山和地球内部研究中心(VERC),海洋地球动力学研究所(IMG),日本地球科学和技术部门的(JAMSTEC),***日本千叶大学理科研究生院,日本千叶263-8522 ****日本横滨236-0001,日本海洋地球动力学研究所,日本俯冲动力学研究中心(SDR) *****日本东京工业大学地球与行星科学系,东京152-8550 ******高知岩心样品研究所日本海洋地球科学技术振兴院(JAMSTEC)超尖端科学技术先锋研究所,日本南国,783-8502 *******千叶大学科学与工程研究生院,日本千叶,263-8522。地理学报,130(4)559-584 2021 doi:10.5026/jgeography.130.559
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Testing the Ontong Java Nui Hypothesis: The Largest Supervolcano Ever on Earth
Large Igneous Provinces (LIPs), such as the Ontong Java Plateau (OJP) in the western equatorial Pacific, provide information on mantle processes and composition, and their formation may have global environmental consequences. The OJP is the largest oceanic plateau and is probably the most voluminous igneous edifice on Earth. Despite its importance, the size, volume, and formation rate of the OJP are not yet well constrained. The maximum extent of OJP-related volcanism may be even greater than currently estimated, because volcanological studies indicate that long lava flows (or sills) from the OJP may have reached the adjacent Nauru, East Mariana, and possibly Pigafetta basins. Moreover, the similarity in age and some geochemistry of lavas from the Ontong Java, Hikurangi, and Manihiki plateaus suggests that they once may have been part of a single LIP (Ontong Java Nui, OJN). If true, the massive volcanism may have covered * 国立科学博物館地学研究部 ** 海洋研究開発機構海域地震火山部門火山・地球内部研究センター *** 千葉大学大学院理学研究院 **** 海洋研究開発機構海域地震火山部門地震発生帯研究センター ***** 東京工業大学地球惑星科学系 ****** 海洋研究開発機構超先鋭研究開発部門高知コア研究所 ******* 千葉大学大学院融合理工学府 * Department of Geology and Paleontology, National Museum of Nature and Science, Tsukuba, 305-0005, Japan ** Volcanoes and Earth’s Interior Research Center (VERC), Research Institute for Marine Geodynamics (IMG), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, 237-0061, Japan *** Graduate School of Science, Chiba University, Chiba 263-8522, Japan **** Subduction Dynamics Research Center (SDR), Research Institute for Marine Geodynamics (IMG), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, 236-0001, Japan ***** Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, 152-8550, Japan ****** Kochi Institute for Core Sample Research, Institute for Extra-cutting-edge Science and Technology Avant-garde Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Nankoku, 783-8502, Japan ******* Graduate School of Science and Engineering, Chiba University, Chiba, 263-8522, Japan 地学雑誌 Journal of Geography(Chigaku Zasshi) 130(4)559­584 2021 doi:10.5026/jgeography.130.559
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CiteScore
1.50
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