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夏威夷-天皇海山链5000万年前开始形成,记录了太平洋板块运动的重大变化。

50-Ma initiation of Hawaiian-Emperor bend records major change in Pacific plate motion.

作者信息

Sharp Warren D, Clague David A

机构信息

Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA.

出版信息

Science. 2006 Sep 1;313(5791):1281-4. doi: 10.1126/science.1128489.

Abstract

The Hawaiian-Emperor bend has played a prominent yet controversial role in deciphering past Pacific plate motions and the tempo of plate motion change. New ages for volcanoes of the central and southern Emperor chain define large changes in volcanic migration rate with little associated change in the chain's trend, which suggests that the bend did not form by slowing of the Hawaiian hot spot. Initiation of the bend near Kimmei seamount about 50 million years ago (MA) was coincident with realignment of Pacific spreading centers and early magmatism in western Pacific arcs, consistent with formation of the bend by changed Pacific plate motion.

摘要

夏威夷-帝王海山链在解读过去太平洋板块运动及板块运动速率变化的节奏方面扮演了重要但颇具争议的角色。帝王海山链中部和南部火山的新年代测定显示,火山迁移速率发生了巨大变化,而海山链走向的相关变化却很小,这表明该弯曲并非由夏威夷热点的减速形成。约5000万年前,在金美名海山附近开始出现弯曲,这与太平洋扩张中心的重新排列以及西太平洋岛弧的早期岩浆活动同时发生,这与太平洋板块运动变化导致弯曲形成的观点相符。

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