Progress in palaeotsunami research

被引:235
作者
Goff, James [1 ,2 ]
Chague-Goff, Catherine [1 ,2 ,3 ]
Nichol, Scott [4 ]
Jaffe, Bruce [5 ]
Dominey-Howes, Dale [1 ,2 ]
机构
[1] Univ New S Wales, Australia Pacific Tsunami Res Ctr, Sydney, NSW 2052, Australia
[2] Univ New S Wales, Nat Hazards Res Lab, Sch Biol Earth & Environm Sci, Sydney, NSW 2052, Australia
[3] Australian Nucl & Sci Technol Org, Inst Environm Res, Kirrawee Dc, NSW 2232, Australia
[4] Geosci Australia, Canberra, ACT 2601, Australia
[5] US Geol Survey, Pacific Coastal & Marine Sci Ctr, Santa Cruz, CA 95060 USA
关键词
Palaeotsunami; Geology; Geomorphology; Archaeology; Microfossils; Geochemistry; INDIAN-OCEAN TSUNAMI; SOUTH-PACIFIC TSUNAMI; DECEMBER; 2004; TSUNAMI; LAND-LEVEL CHANGES; NEW-ZEALAND; ENVIRONMENTAL-CHANGES; HOLOCENE TSUNAMIS; NATIONAL-PARK; COASTAL ZONE; SEA-LEVEL;
D O I
10.1016/j.sedgeo.2011.11.002
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The study of palaeotsunamis preserved in the sedimentary record has developed over the past three decades to a point where the criteria used to identify these events range from well-tested and accepted to new methods yet to receive wide application. In this paper we review progress with the development of these criteria and identify opportunities for refinements and for extending their application to new settings. The emphasis here is on promoting the use of multiple proxies, selected to best match the context of the site or region of interest. Ultimately, this requires that palaeotsunami research must be a multidisciplinary endeavour and indeed, extend beyond the geological sciences of sedimentology and stratigraphy and, to include knowledge and approaches from field such as archaeology, anthropology and sociology. We also argue that in some instances, despite the use of multiple proxies, the evidence for tsunami inundation of a coast simply may not be preserved. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:70 / 88
页数:19
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