Highly variable recurrence of tsunamis in the 7,400 years before the 2004 Indian Ocean tsunami

被引:89
作者
Rubin, Charles M. [1 ,2 ]
Horton, Benjamin P. [1 ,2 ,3 ]
Sieh, Kerry [1 ,2 ]
Pilarczyk, Jessica E. [4 ]
Daly, Patrick [1 ]
Ismail, Nazli [5 ]
Parnell, Andrew C. [6 ]
机构
[1] Nanyang Technol Univ, Earth Observ Singapore, Singapore 639798, Singapore
[2] Nanyang Technol Univ, Asian Sch Environm, Singapore 639798, Singapore
[3] Rutgers State Univ, Dept Marine & Coastal Sci, New Brunswick, NJ 08901 USA
[4] Univ Southern Mississippi, Stennis Space Ctr, Div Marine Sci, Hattiesburg, MS 39529 USA
[5] Syiah Kuala Univ, Fac Math & Nat Sci, Dept Phys Geophys, Banda Aceh 23111, Indonesia
[6] Univ Coll Dublin, Sch Math & Stat, Insight Ctr Data Analyt, Dublin D04 V1W8 4, Ireland
基金
美国国家科学基金会; 新加坡国家研究基金会;
关键词
PHRA THONG ISLAND; SEA-LEVEL; EARTHQUAKES; DEPOSITS; COAST; ACEH; ENVIRONMENTS; FORAMINIFERA; INDICATORS; SUBSIDENCE;
D O I
10.1038/ncomms16019
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The devastating 2004 Indian Ocean tsunami caught millions of coastal residents and the scientific community off-guard. Subsequent research in the Indian Ocean basin has identified prehistoric tsunamis, but the timing and recurrence intervals of such events are uncertain. Here we present an extraordinary 7,400 year stratigraphic sequence of prehistoric tsunami deposits from a coastal cave in Aceh, Indonesia. This record demonstrates that at least 11 prehistoric tsunamis struck the Aceh coast between 7,400 and 2,900 years ago. The average time period between tsunamis is about 450 years with intervals ranging from a long, dormant period of over 2,000 years, to multiple tsunamis within the span of a century. Although there is evidence that the likelihood of another tsunamigenic earthquake in Aceh province is high, these variable recurrence intervals suggest that long dormant periods may follow Sunda megathrust ruptures as large as that of the 2004 Indian Ocean tsunami.
引用
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页数:12
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