Submergence and uplift associated with the giant 1833 Sumatran subduction earthquake : evidence from coral microatolls
The giant Sumatran subduction earthquake of 1833 appears as a large emergence event in fossil coral microatolls on the reefs of Sumatra's outer-arc ridge. Stratigraphic analysis of these and living microatolls nearby allow us to estimate that 1833 emergence increased trenchward from about 1 to...
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Main Authors: | , , , , |
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格式: | Article |
語言: | English |
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2012
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在線閱讀: | https://hdl.handle.net/10356/95448 http://hdl.handle.net/10220/8492 |
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機構: | Nanyang Technological University |
語言: | English |