The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes
Eustasy and glacio- and hydro-isostatic adjustment are the main drivers of regional variability of Holocene relative sea-level (RSL) records. These regional variations in Holocene RSL influence the preservation of coastal wetland stratigraphic records of prehistoric earthquakes along subduction zone...
| Main Authors: | , , , , , , |
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| Other Authors: | |
| Format: | Journal Article |
| Language: | English |
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2021
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| Online Access: | https://hdl.handle.net/10356/146615 |
| _version_ | 1826119191419158528 |
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| author | Dura, Tina Engelhart, Simon E. Vacchi, Matteo Horton, Benjamin Peter Kopp, Robert E. Peltier, W. Richard Bradley, Sarah |
| author2 | Asian School of the Environment |
| author_facet | Asian School of the Environment Dura, Tina Engelhart, Simon E. Vacchi, Matteo Horton, Benjamin Peter Kopp, Robert E. Peltier, W. Richard Bradley, Sarah |
| author_sort | Dura, Tina |
| collection | NTU |
| description | Eustasy and glacio- and hydro-isostatic adjustment are the main drivers of regional variability of Holocene relative sea-level (RSL) records. These regional variations in Holocene RSL influence the preservation of coastal wetland stratigraphic records of prehistoric earthquakes along subduction zone coasts. The length and completeness of prehistoric earthquake records is intrinsically linked to the accommodation space provided by gradually rising (<3 mm/year) Holocene RSL. In near-field regions that were located beneath northern hemisphere ice sheets (e.g., western Vancouver Island), RSL fall from a mid-Holocene highstand has limited prehistoric earthquake records to the last 1 ka. In intermediate field regions (e.g., southern Washington and central Oregon), gradual RSL rise over the last ∼7 ka has preserved widespread records of prehistoric earthquakes. In far-field regions (e.g., Sumatra, Chile, and Japan), fragmentary stratigraphic evidence of prehistoric earthquakes has been preserved only during periods of gradual RSL rise prior to a mid-Holocene highstand, or during the last 1–3 ka, when RSL was within 2 m of modern sea level, and thus within the tidal frame. |
| first_indexed | 2024-10-01T04:56:07Z |
| format | Journal Article |
| id | ntu-10356/146615 |
| institution | Nanyang Technological University |
| language | English |
| last_indexed | 2024-10-01T04:56:07Z |
| publishDate | 2021 |
| record_format | dspace |
| spelling | ntu-10356/1466152021-03-03T03:23:23Z The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes Dura, Tina Engelhart, Simon E. Vacchi, Matteo Horton, Benjamin Peter Kopp, Robert E. Peltier, W. Richard Bradley, Sarah Asian School of the Environment Earth Observatory of Singapore Science::Physics Relative Sea Level Glacio-isostatic Adjustment Eustasy and glacio- and hydro-isostatic adjustment are the main drivers of regional variability of Holocene relative sea-level (RSL) records. These regional variations in Holocene RSL influence the preservation of coastal wetland stratigraphic records of prehistoric earthquakes along subduction zone coasts. The length and completeness of prehistoric earthquake records is intrinsically linked to the accommodation space provided by gradually rising (<3 mm/year) Holocene RSL. In near-field regions that were located beneath northern hemisphere ice sheets (e.g., western Vancouver Island), RSL fall from a mid-Holocene highstand has limited prehistoric earthquake records to the last 1 ka. In intermediate field regions (e.g., southern Washington and central Oregon), gradual RSL rise over the last ∼7 ka has preserved widespread records of prehistoric earthquakes. In far-field regions (e.g., Sumatra, Chile, and Japan), fragmentary stratigraphic evidence of prehistoric earthquakes has been preserved only during periods of gradual RSL rise prior to a mid-Holocene highstand, or during the last 1–3 ka, when RSL was within 2 m of modern sea level, and thus within the tidal frame. 2021-03-03T03:23:23Z 2021-03-03T03:23:23Z 2016 Journal Article Dura, T., Engelhart, S. E., Vacchi, M., Horton, B. P., Kopp, R. E., Peltier, W. R., & Bradley, S. (2016). The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes. Current Climate Change Reports, 2(3), 86-100. doi:10.1007/s40641-016-0041-y 2198-6061 https://hdl.handle.net/10356/146615 10.1007/s40641-016-0041-y 2-s2.0-85013937431 3 2 86 100 en Current Climate Change Reports © 2016 Springer International Publishing AG. All rights reserved. |
| spellingShingle | Science::Physics Relative Sea Level Glacio-isostatic Adjustment Dura, Tina Engelhart, Simon E. Vacchi, Matteo Horton, Benjamin Peter Kopp, Robert E. Peltier, W. Richard Bradley, Sarah The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes |
| title | The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes |
| title_full | The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes |
| title_fullStr | The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes |
| title_full_unstemmed | The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes |
| title_short | The role of Holocene relative sea-level change in preserving records of subduction zone earthquakes |
| title_sort | role of holocene relative sea level change in preserving records of subduction zone earthquakes |
| topic | Science::Physics Relative Sea Level Glacio-isostatic Adjustment |
| url | https://hdl.handle.net/10356/146615 |
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