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太平洋板块运动变化导致了夏威夷-皇帝海山链弯曲。

Pacific plate motion change caused the Hawaiian-Emperor Bend.

机构信息

Centre for Earth Evolution and Dynamics (CEED), University of Oslo, 0315 Oslo, Norway.

Helmholtz Centre Potsdam, GFZ, Telegrafenberg, 14473 Potsdam, Germany.

出版信息

Nat Commun. 2017 Jun 5;8:15660. doi: 10.1038/ncomms15660.

DOI:10.1038/ncomms15660
PMID:28580950
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5465363/
Abstract

A conspicuous 60° bend of the Hawaiian-Emperor Chain in the north-western Pacific Ocean has variously been interpreted as the result of an abrupt Pacific plate motion change in the Eocene (∼47 Ma), a rapid southward drift of the Hawaiian hotspot before the formation of the bend, or a combination of these two causes. Palaeomagnetic data from the Emperor Seamounts prove ambiguous for constraining the Hawaiian hotspot drift, but mantle flow modelling suggests that the hotspot drifted 4-9° south between 80 and 47 Ma. Here we demonstrate that southward hotspot drift cannot be a sole or dominant mechanism for formation of the Hawaiian-Emperor Bend (HEB). While southward hotspot drift has resulted in more northerly positions of the Emperor Seamounts as they are observed today, formation of the HEB cannot be explained without invoking a prominent change in the direction of Pacific plate motion around 47 Ma.

摘要

北太平洋夏威夷-皇帝海山链的一个明显的 60°弯曲,各种解释为始新世(约 47Ma)太平洋板块运动的突然变化,或弯曲形成前夏威夷热点的快速向南漂移,或这两种原因的组合。来自皇帝海山的古地磁数据对约束夏威夷热点漂移模棱两可,但地幔流模拟表明,热点在 80 至 47Ma 期间向南漂移了 4-9°。在这里,我们证明了热点的向南漂移不能是形成夏威夷-皇帝弯曲(HEB)的唯一或主要机制。虽然热点的向南漂移导致了今天观察到的皇帝海山更偏北的位置,但如果不引入 47Ma 左右太平洋板块运动方向的明显变化,就无法解释 HEB 的形成。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/7c679a203a5c/ncomms15660-f8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/5c1547f57f38/ncomms15660-f1.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/651bc1535d89/ncomms15660-f3.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/86b0007d7c00/ncomms15660-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/f6f0b732fc75/ncomms15660-f6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/d13f17596bff/ncomms15660-f7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/7c679a203a5c/ncomms15660-f8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/5c1547f57f38/ncomms15660-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/0c70c0f1c6d4/ncomms15660-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/651bc1535d89/ncomms15660-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/0c332ebe0a42/ncomms15660-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/86b0007d7c00/ncomms15660-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/f6f0b732fc75/ncomms15660-f6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/d13f17596bff/ncomms15660-f7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7b42/5465363/7c679a203a5c/ncomms15660-f8.jpg

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本文引用的文献

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2
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Nature. 2016 May 12;533(7602):239-42. doi: 10.1038/nature17422.
3
Intra-oceanic subduction shaped the assembly of Cordilleran North America.大洋内俯冲作用塑造了科迪勒拉北美洲的聚合。
Innovation (Camb). 2023 Feb 22;4(2):100404. doi: 10.1016/j.xinn.2023.100404. eCollection 2023 Mar 13.
4
Hotspot motion caused the Hawaiian-Emperor Bend and LLSVPs are not fixed.热点运动导致夏威夷-皇帝弯曲和 LLSVPs 不固定。
Nat Commun. 2019 Jul 29;10(1):3370. doi: 10.1038/s41467-019-11314-6.
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Nat Commun. 2018 Feb 27;9(1):854. doi: 10.1038/s41467-018-03277-x.
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Intraoceanic subduction spanned the Pacific in the Late Cretaceous-Paleocene.大洋内俯冲作用横跨晚白垩世-古新世时期的太平洋。
Sci Adv. 2017 Nov 8;3(11):eaao2303. doi: 10.1126/sciadv.aao2303. eCollection 2017 Nov.
Nature. 2013 Apr 4;496(7443):50-6. doi: 10.1038/nature12019.
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The bent Hawaiian-Emperor hotspot track: inheriting the mantle wind.弯曲的夏威夷-天皇热点轨迹:承袭地幔风。
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6
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Science. 2003 Aug 22;301(5636):1064-9. doi: 10.1126/science.1086442. Epub 2003 Jul 24.