1605年琼州大地震陆陷成海和可能的海啸

徐起浩

1605年琼州大地震陆陷成海和可能的海啸

徐起浩

广东省地震局, 广东, 广州, 510070

基金项目: 广东省科技计划资助项目(32606)

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出版历程
- 收稿日期: 2005-12-28
- 修回日期: 2006-08-28

The land sank into the sea and possible tsunami by the great earthquake in Qiongzhou in China in 1605

XU Qi-hao

Earthquake Administration of Guangdong Province, Guangzhou 510070, China

摘要

摘要: 海啸通常分近海海啸和远洋海啸.近海海啸发生在近岸数十千米或一二百千米以内的海底,而远洋海啸是从数百千米至数千千米外的远洋或横越大洋传播过来的海啸^[1].据我国研究者统计,我国有记载以来共记录了26次地震海啸,其中造成损失的破坏性海啸至少有8~9次^[2].20世纪80年代以前国外较多研究者和国内研究者大都主要研究和论述近海地震海啸和远洋传播的地震海啸及给海岸带带来的灾害和影响^[3,4].虽然我国地震工作者早在20世纪70年代末就已经在文献中论述过琼州大地震极震区一些海岸陆陷成海^[5,6],其后又有多人对这次大地震陆陷成海进行过进一步深入研究^[7~21],但都未明确与海啸之联系.
- 史料记载 /
- 海底废墟 /
- 陆陷成海地震地貌 /
- 东寨港 /
- 海啸
- historical data /
- ruins in the seafloor earthquake landform of the land sinking into the sea /
- Dongzhaigang Bay /
- tsunami /

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参考文献(51)

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