Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology
The extent and controls of long-term elastic strength and seismicity in the upper continental lithospheric mantle (UCLM) are controversial topics in continental tectonics. One key issue is the scarcity of UCLM earthquakes, even where the UCLM is likely to be colder than 600°C. The rarity of these ea...
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| Format: | Journal article |
| Language: | English |
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2012
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| _version_ | 1797061489830395904 |
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| author | Sloan, R Jackson, J |
| author_facet | Sloan, R Jackson, J |
| author_sort | Sloan, R |
| collection | OXFORD |
| description | The extent and controls of long-term elastic strength and seismicity in the upper continental lithospheric mantle (UCLM) are controversial topics in continental tectonics. One key issue is the scarcity of UCLM earthquakes, even where the UCLM is likely to be colder than 600°C. The rarity of these earthquakes could be because the UCLM generally relatively hydrous causing it to deform aseismically even when colder than 600°C, unless it is deforming at exceptionally high strain rates. Alternatively, the UCLM could be relatively anhydrous, and potentially seismogenic at temperatures below 600°C; in which case the rarity of UCLM earthquakes may be because areas where the UCLM is colder than 600°C have such a thick seismogenic layer, and such a cool mantle root, that they deform exceptionally slowly. The identification and study of UCLM earthquakes allows us to distinguish between these possibilities. Here we show that two earthquakes occurred in the UCLM beneath the epicontinental Arafura Sea. Both earthquakes occurred where the UCLM is probably cooler than 600°C and one of these earthquakes lies -25 km below the Moho in an region where there is no evidence of unusually high strain rates. There at least, it is probable that the UCLM is relatively anhydrous, and seismogenic at temperatures below 600°C. We also find evidence that regions where the UCLM is colder than 600°C also have a seismogenic lower crust. This results in a single, extremely strong layer comprising the entire crust and the UCLM down to the 600°C isotherm. © 2012 by the American Geophysical Union. |
| first_indexed | 2024-03-06T20:31:54Z |
| format | Journal article |
| id | oxford-uuid:31561073-c3e5-49c9-97de-4a5c2a827c90 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-06T20:31:54Z |
| publishDate | 2012 |
| record_format | dspace |
| spelling | oxford-uuid:31561073-c3e5-49c9-97de-4a5c2a827c902022-03-26T13:07:16ZUpper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheologyJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:31561073-c3e5-49c9-97de-4a5c2a827c90EnglishSymplectic Elements at Oxford2012Sloan, RJackson, JThe extent and controls of long-term elastic strength and seismicity in the upper continental lithospheric mantle (UCLM) are controversial topics in continental tectonics. One key issue is the scarcity of UCLM earthquakes, even where the UCLM is likely to be colder than 600°C. The rarity of these earthquakes could be because the UCLM generally relatively hydrous causing it to deform aseismically even when colder than 600°C, unless it is deforming at exceptionally high strain rates. Alternatively, the UCLM could be relatively anhydrous, and potentially seismogenic at temperatures below 600°C; in which case the rarity of UCLM earthquakes may be because areas where the UCLM is colder than 600°C have such a thick seismogenic layer, and such a cool mantle root, that they deform exceptionally slowly. The identification and study of UCLM earthquakes allows us to distinguish between these possibilities. Here we show that two earthquakes occurred in the UCLM beneath the epicontinental Arafura Sea. Both earthquakes occurred where the UCLM is probably cooler than 600°C and one of these earthquakes lies -25 km below the Moho in an region where there is no evidence of unusually high strain rates. There at least, it is probable that the UCLM is relatively anhydrous, and seismogenic at temperatures below 600°C. We also find evidence that regions where the UCLM is colder than 600°C also have a seismogenic lower crust. This results in a single, extremely strong layer comprising the entire crust and the UCLM down to the 600°C isotherm. © 2012 by the American Geophysical Union. |
| spellingShingle | Sloan, R Jackson, J Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology |
| title | Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology |
| title_full | Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology |
| title_fullStr | Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology |
| title_full_unstemmed | Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology |
| title_short | Upper-mantle earthquakes beneath the arafura sea and south aru trough: Implications for continental rheology |
| title_sort | upper mantle earthquakes beneath the arafura sea and south aru trough implications for continental rheology |
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