| _version_ | 1867170125347553280 |
|---|---|
| author | Cornard, Pauline Dawson, Harriet Pickering, Kevin T |
| author_facet | Cornard, Pauline Dawson, Harriet Pickering, Kevin T |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | U-Pb zircon age dating was applied on U-channel samples (30cc) that were collected from sandy deposits in cores from IODP Site C0024 (one sample; frontal Nankai accretionary Prism), ODP Site 1177 (two samples; Western Shikoku Basin) and IODP sites C0011 (three samples) and C0012 (one sample; Eastern Shikoku Basin). Detrital zircon U-Pb ages were measured using the London Thermochronology Research Group facilities at UCL based on a New Wave Nd: YAG 213 nm laser ablation system coupled plasma-mass spectrometry. Real time U-Pb were processed using GLITTER data reduction software. Repeated measurements of external zircon standard Plesovice (TIMS reference 337.13 +/-0.37 Myr ago) and NIST 612 silicate glass were used to correct for instrumental mass bias and depth-dependent inter-element fractionation of Pb, Th, and U. 206Pb/238U ages are used for those grain younger than 1 Ga, and for zircon grains older than 1,000 Ma we used the 207Pb/206Pb ages to determine the crystallization age. To better constrain the sediment provenance along the Nankai subduction zone, we integrated published U-Pb zircon age to our study. These include (1) potential sediment sources, e.g., Nagara, Yodo, Tenryu, Kiso and Fuji rivers from Clift et al. (2013) (https://doi.pangaea.de/10.1002/tect.20033), the Yangtze and Yellow rivers from Huang et al. (2020) (https://doi.pangaea.de/10.3390/min10050398), the Shimanto Complex from Shibata et al. (2008) (https://doi.org/10.1111/j.1440-1738.2008.00626.x) and the Sanbagawa Belt from Tsutsumi et al. (2009) (https://doi.org/10.2465/jmps.080416) and (2) published zircon ages from the frontal accretionary prism ((ODP sites 1176 and 1177 and IODP sites C0006E and C0007E; Clift et al., 2013) (https://doi.pangaea.de/10.1002/tect.20033). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_969327 |
| institution | PANGAEA |
| language | en |
| publishDate | 2024 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Detrital zircon U/Pb ages from the Nankai subduction zone (Japan) Cornard, Pauline Dawson, Harriet Pickering, Kevin T 190-1177A; 322-C0011B; 322-C0012A; 358-C0024D; Age; Age, 206Pb/238U Lead-Uranium; Age, 207Pb/206Pb Lead-Lead; Age, 207Pb/235U Lead-Uranium; Age, dated; Age, dated standard error; Age, standard error; Chikyu; deep-marine sediments; DEPTH, sediment/rock; DRILL; Drilling/coring; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp322; Exp358; GLITTER - data reduction software; Grains; IODP Depth Scale Terminology; Joides Resolution; Latitude of event; Lead-206/Uranium-238 ratio; Lead-206/Uranium-238 ratio, standard error; Lead-207/Lead-206 ratio; Lead-207/Lead-206 ratio, standard error; Lead-207/Uranium-235 ratio; Lead-207/Uranium-235 ratio, standard error; Leg190; Longitude of event; NanTroSEIZE Plate Boundary Deep Riser 4; NanTroSEIZE Stage 2: Subduction Input; Percentage; petrography analysis; Philippine Sea; Sample code/label; Thorium; Thorium/Uranium ratio; Uranium; zircon age dating U-Pb zircon age dating was applied on U-channel samples (30cc) that were collected from sandy deposits in cores from IODP Site C0024 (one sample; frontal Nankai accretionary Prism), ODP Site 1177 (two samples; Western Shikoku Basin) and IODP sites C0011 (three samples) and C0012 (one sample; Eastern Shikoku Basin). Detrital zircon U-Pb ages were measured using the London Thermochronology Research Group facilities at UCL based on a New Wave Nd: YAG 213 nm laser ablation system coupled plasma-mass spectrometry. Real time U-Pb were processed using GLITTER data reduction software. Repeated measurements of external zircon standard Plesovice (TIMS reference 337.13 +/-0.37 Myr ago) and NIST 612 silicate glass were used to correct for instrumental mass bias and depth-dependent inter-element fractionation of Pb, Th, and U. 206Pb/238U ages are used for those grain younger than 1 Ga, and for zircon grains older than 1,000 Ma we used the 207Pb/206Pb ages to determine the crystallization age. To better constrain the sediment provenance along the Nankai subduction zone, we integrated published U-Pb zircon age to our study. These include (1) potential sediment sources, e.g., Nagara, Yodo, Tenryu, Kiso and Fuji rivers from Clift et al. (2013) (https://doi.pangaea.de/10.1002/tect.20033), the Yangtze and Yellow rivers from Huang et al. (2020) (https://doi.pangaea.de/10.3390/min10050398), the Shimanto Complex from Shibata et al. (2008) (https://doi.org/10.1111/j.1440-1738.2008.00626.x) and the Sanbagawa Belt from Tsutsumi et al. (2009) (https://doi.org/10.2465/jmps.080416) and (2) published zircon ages from the frontal accretionary prism ((ODP sites 1176 and 1177 and IODP sites C0006E and C0007E; Clift et al., 2013) (https://doi.pangaea.de/10.1002/tect.20033). |
| title | Detrital zircon U/Pb ages from the Nankai subduction zone (Japan) |
| topic | 190-1177A; 322-C0011B; 322-C0012A; 358-C0024D; Age; Age, 206Pb/238U Lead-Uranium; Age, 207Pb/206Pb Lead-Lead; Age, 207Pb/235U Lead-Uranium; Age, dated; Age, dated standard error; Age, standard error; Chikyu; deep-marine sediments; DEPTH, sediment/rock; DRILL; Drilling/coring; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp322; Exp358; GLITTER - data reduction software; Grains; IODP Depth Scale Terminology; Joides Resolution; Latitude of event; Lead-206/Uranium-238 ratio; Lead-206/Uranium-238 ratio, standard error; Lead-207/Lead-206 ratio; Lead-207/Lead-206 ratio, standard error; Lead-207/Uranium-235 ratio; Lead-207/Uranium-235 ratio, standard error; Leg190; Longitude of event; NanTroSEIZE Plate Boundary Deep Riser 4; NanTroSEIZE Stage 2: Subduction Input; Percentage; petrography analysis; Philippine Sea; Sample code/label; Thorium; Thorium/Uranium ratio; Uranium; zircon age dating |
| url | https://doi.org/10.1594/PANGAEA.969327 |