U-Th systematics and ages of carbonate chimneys at the Lost City Hydrothermal Field

TitleU-Th systematics and ages of carbonate chimneys at the Lost City Hydrothermal Field
Publication TypeJournal Article
Year of Publication2011
AuthorsLudwig, KA, Shen, CC, Kelley, DS, Cheng, H, Edwards, RL
JournalGeochimica et Cosmochimica Acta
Volume75
Pagination1869–1888
ISSN0016-7037
KeywordsHOV 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

URLhttp://dx.doi.org/10.1016/j.gca.2011.01.008
DOI10.1016/j.gca.2011.01.008