(Table 1) U and Th isotope analyses of pyrite and anhydrite of ODP Site 158-957

• Main Authors: You, Chen-Feng, Bickle, Michael J
• Format: Dataset
• Language: English
• Published: PANGAEA 1998
• Subjects: 158-957C; 158-957E; 158-957G; 158-957H; 158-957I; 158-957K; 158-957M; Age; 234U/230Th Uranium-Thorium; dated; dated standard deviation; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg158; Mineral name; North Atlantic Ocean; Ocean Drilling Program; ODP; Sample code/label; Thermal Ionization Mass Spectrometry (TIMS); Thorium; error; relative; Thorium-230/Uranium-238; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 ratio; Uranium; Uranium-234/Uranium-238 activity ratio; Mid-Atlantic Ridge; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.769877; https://doi.org/10.1594/PANGAEA.769877

Hydrothermal circulation at oceanic spreading ridges causes sea water to penetrate to depths of 2 to 3 km in the oceanic crust where it is heated to ~400 °C before venting at spectacular 'black smokers'. These hydrothermal systems exert a strong influence on ocean chemistry (Edmond et al., 1979, doi:10.1016/0012-821X(79)90061-X), yet their structure, longevity and magnitude remain largely unresolved (Elderfield and Schultz., 1996, doi:10.1146/annurev.earth.24.1.191). The active Transatlantic Geotraverse (TAG) deposit, at 26° N on the Mid-Atlantic Ridge, is one of the largest, oldest and most intensively studied of the massive sulphide mounds that accumulate beneath black-smoker fields. Here we report ages of sulphides and anhydrites from the recently drilled (Humphris et al., 1995, doi:10.1038/377713a0) TAG substrate structures -determined from 234U-230Th systematics analysed by thermal ionization mass spectrometry. The new precise ages combined with existing data (Lalou et al., 1993, doi:10.1029/92JB01898; 1998, doi:10.2973/odp.proc.sr.158.214.1998) show that the oldest material (11,000 to 37,000 years old) forms a layer across the centre of the deposit with younger material (2,300–7,800 years old) both above and below. This stratigraphy confirms that much of the sulphide and anhydrite are precipitated within the mound by mixing of entrained sea water with hydrothermal fluid (James and Elderfield, 1996, doi:10.1130/0091-7613(1996)024<1147:COOFFA>2.3.CO;2). The age distribution is consistent with episodic activity of the hydrothermal system recurring at intervals of up to 2,000 years.