Title | U-Th systematics and ages of carbonate chimneys at the Lost City Hydrothermal Field |
Publication Type | Journal Article |
Year of Publication | 2011 |
Authors | Ludwig, KA, Shen, CC, Kelley, DS, Cheng, H, Edwards, RL |
Journal | Geochimica et Cosmochimica Acta |
Volume | 75 |
Pagination | 1869–1888 |
ISSN | 0016-7037 |
Keywords | HOV Alvin (Human Occupied Vehicle) |
Abstract | The Lost City Hydrothermal Field (LCHF) is a serpentinite-hosted vent field located 15 km west of the spreading axis of the Mid-Atlantic Ridge. In this study, uranium–thorium (U–Th) geochronological techniques have been used to examine the U–Th systematics of hydrothermal fluids and the 230Th ages of hydrothermally-precipitated carbonate chimneys at the LCHF. Fluid sample analyses indicate that endmember fluids likely contain only 0.0073 ng/g U or less compared to 3.28 ± 0.03 ng/g of U in ambient seawater. For fluid samples containing only 2–21{%} ambient seawater (1.1–11 mmol/kg Mg), Th concentration is 0.11–0.13 pg/g and surrounding seawater concentrations average 0.133 ± 0.016 pg/g. The 230Th/232Th atomic ratios of the vent fluids range from 1 (±10) × 10−6 to 11 (±5) × 10−6, are less than those of seawater, and indicate that the vent fluids may contribute a minor amount of non-radiogenic 230Th to the LCHF carbonate chimney deposits. Chimney 238U concentrations range from 1 to 10 $μ$g/g and the average chimney corrected initial $δ$234U is 147.2 ± 0.8, which is not significantly different from the ambient seawater value of 146.5 ± 0.6. Carbonate 232Th concentrations range broadly from 0.0038 ± 0.0003 to 125 ± 16 ng/g and 230Th/232Th atomic ratios vary from near seawater values of 43 (±8) × 10−6 up to 530 (±25) × 10−3. Chimney ages, corrected for initial 230Th, range from 17 ± 6 yrs to 120 ± 13 kyrs. The youngest chimneys are at the intersection of two active, steeply-dipping normal faults that cut the Atlantis Massif; the oldest chimneys are located in the southwest portion of the field. Vent deposits on a steep, fault-bounded wall on the east side of the field are all Th, range from 17 ± 6 yrs to 120 ± 13 kyrs. The youngest chimneys are at the intersection of two active, steeply-dipping normal faults that cut the Atlantis Massif; the oldest chimneys are located in the southwest portion of the field. Vent deposits on a steep, fault-bounded wall on the east side of the field are all |
URL | http://dx.doi.org/10.1016/j.gca.2011.01.008 |
DOI | 10.1016/j.gca.2011.01.008 |