Major element composition of IODP Site U1501 in the South China Sea from 5.2 to 5.8 Ma
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| Autores principales: | , , |
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
2021
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| _version_ | 1867170111041830912 |
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| author | Hu, Zhe Huang, Baoqi Geng, Li |
| author_facet | Hu, Zhe Huang, Baoqi Geng, Li |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | IODP Site U1501 (18°53.09′N, 115°45.95′E, water depth: 2846 m) is situated on the west side of Pearl River Canyon. The length for hole C at IODP Site U1501 is up to 461.8 m, covering the last 40 Ma (Jian et al., 2018; Ma et al., 2019). 31 samples were selected at 20 cm intervals from the interval from 92.86 to 99.29 m, which spans from 5.2-5.8 Ma (Jian et al., 2018). All 31 samples of IODP Site U1501 are analyzed by inductively coupled plasma-optical emission (ICP-OES) to acquire the major elemental contents in Peking University during June 2021. We use the major element data to calculate the provenance proxies (Hu et al., 2021), then further discuss the change of Taiwan input during the late Miocene. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_937324 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Major element composition of IODP Site U1501 in the South China Sea from 5.2 to 5.8 Ma Hu, Zhe Huang, Baoqi Geng, Li 368-U1501C; AGE; Aluminium oxide; Calcium oxide; deep sea sediment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp368; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Late Miocene; Magnesium oxide; Major element; Phosphorus pentoxide; Potassium oxide; Sodium oxide; South China Sea; Titanium dioxide IODP Site U1501 (18°53.09′N, 115°45.95′E, water depth: 2846 m) is situated on the west side of Pearl River Canyon. The length for hole C at IODP Site U1501 is up to 461.8 m, covering the last 40 Ma (Jian et al., 2018; Ma et al., 2019). 31 samples were selected at 20 cm intervals from the interval from 92.86 to 99.29 m, which spans from 5.2-5.8 Ma (Jian et al., 2018). All 31 samples of IODP Site U1501 are analyzed by inductively coupled plasma-optical emission (ICP-OES) to acquire the major elemental contents in Peking University during June 2021. We use the major element data to calculate the provenance proxies (Hu et al., 2021), then further discuss the change of Taiwan input during the late Miocene. |
| title | Major element composition of IODP Site U1501 in the South China Sea from 5.2 to 5.8 Ma |
| topic | 368-U1501C; AGE; Aluminium oxide; Calcium oxide; deep sea sediment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp368; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Late Miocene; Magnesium oxide; Major element; Phosphorus pentoxide; Potassium oxide; Sodium oxide; South China Sea; Titanium dioxide |
| url | https://doi.org/10.1594/PANGAEA.937324 |