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Title: Mass spectrometric sup 230 Th- sup 234 U- sup 238 U dating of the Devils Hole calcite vein

Journal Article · · Science (Washington, D.C.); (United States)
; ; ;  [1]; ;  [2];  [3]
  1. U.S. Geological Survey, Denver, CO (United States)
  2. U.S. Geological Survey, Reston, VA (United States)
  3. U.S. Geological Survey, Carson City, NV (United States)

The Devils Hole calcite vein contains a long-term climatic record, but requires accurate chronologic control for its interpretation. Mass-spectrometric U-series ages for samples from core DH-11 yielding {sup 230}Th ages with precisions ranging from less than 1,000 years (2{sigma}) for samples younger than {approximately}140 ka (thousands of years ago) to less than 50,000 years for the oldest samples ({approximately}566 ka). The {sup 234}U/{sup 238}U ages could be determined to a precision of {approximately}20,000 years for all ages. Calcite accumulated continuously from 566 ka until {approximately}60 ka at an average rate of 0.7 millimeter per 10{sup 3} years. The precise agreement between replicate analyses and the concordance of the {sup 230}Th/{sup 238}U and {sup 234}U/{sup 238}U ages for the oldest samples indicate that the DH-11 samples were closed systems and validate the dating technique in general.

OSTI ID:
7225688
Journal Information:
Science (Washington, D.C.); (United States), Vol. 258:5080; ISSN 0036-8075
Country of Publication:
United States
Language:
English