Neon isotope variations in Mid-Atlantic Ridge basalts

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

24

Scientific paper

The isotopic composition of neon was measured for seventeen samples of submarine basalt glass from the Mid-Atlantic Ridge between 54° and 73°N. They include the Reykjanes, Kolbeinsey, and Mohns Ridge segments. Neon isotopic anomalies, relative to the atmospheric ratios, exist in both 20Ne/22Ne and 21Ne/22Ne. A maximum excess 20Ne of 7% was measured in two samples from the Reykjanes Ridge. Samples with lower 20Ne excesses (six samples with δ20Ne between 2 and 4%) from all three ridge segments, appear to result from mixing of a mantle component with a δ20Ne of 7% and atmospheric neon. 21Ne/22Ne ratios are up to 8% above the atmospheric value, with no apparent correlation with the 20Ne excesses. The anomalies in 20Ne/22Ne are difficult to explain by mass fractionation of an atmospheric reservoir since several of the samples have δ20Ne values greater than could be produced by single-stage fractionation. Most likely, the excess 21Ne results from nuclear reactions in the mantle source, although there is no definite correlation between the δ21Ne or the excess 21Ne (cm3 STP/g) and the uranium concentration. Large variations in the observed 4He/20Ne ratio (40-12,000) remain unexplained at this time.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Neon isotope variations in Mid-Atlantic Ridge basalts does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Neon isotope variations in Mid-Atlantic Ridge basalts, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Neon isotope variations in Mid-Atlantic Ridge basalts will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1675367

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.