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| Main Authors: | , , |
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| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
1993
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.785057 |
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| _version_ | 1867168110027472896 |
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| author | Pickering, Kevin T Underwood, Michael B Taira, Asahiko |
| author_facet | Pickering, Kevin T Underwood, Michael B Taira, Asahiko |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The Ocean Drilling Program Leg 131, which drilled in the Nankai Trough in the western Pacific Ocean, has shown for the first time that turbidity currents are deflected and reflected against the trench slopes, such that in the trench outer slope there is a predominant pattern of currents, carrying terrigenous sediments, apparently coming from the open-ocean Shikoku Basin directly toward the trench landward-slope. The purpose of this paper is to summarize the evidence for flow rebound at ODP Leg 131 Site 808, and to show that these results have important implications for the interpretation of paleocurrents in ancient linear turbidite systems. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_785057 |
| institution | PANGAEA |
| language | en |
| publishDate | 1993 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Current ripples from the trench outer slope, ODP Hole 131-808C Pickering, Kevin T Underwood, Michael B Taira, Asahiko -; 131-808C; Correction; Declination; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg131; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; Structure The Ocean Drilling Program Leg 131, which drilled in the Nankai Trough in the western Pacific Ocean, has shown for the first time that turbidity currents are deflected and reflected against the trench slopes, such that in the trench outer slope there is a predominant pattern of currents, carrying terrigenous sediments, apparently coming from the open-ocean Shikoku Basin directly toward the trench landward-slope. The purpose of this paper is to summarize the evidence for flow rebound at ODP Leg 131 Site 808, and to show that these results have important implications for the interpretation of paleocurrents in ancient linear turbidite systems. |
| title | (Table 1) Current ripples from the trench outer slope, ODP Hole 131-808C |
| topic | -; 131-808C; Correction; Declination; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg131; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label; Structure |
| url | https://doi.org/10.1594/PANGAEA.785057 |