Pb isotope compositions of modern deep sea turbidites

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

8

Scientific paper

Modern deep sea turbidite muds and sands collected from Lamont piston cores represent a large range in age of detrital sources as well as a spectrum of tectonic settings. Pb isotope compositions of all but three of the 66 samples lie to the right of the 4.56 Ga Geochron, and most also lie along a slope consistent with a time-integrated κ (232Th/238U) between 3.8 and 4.2. Modern deep sea turbidites show a predictable negative correlation between both Pb and Sr isotope ratios and ɛNd and ɛHf, clearly related to the age of continental sources. However, the consistency between Pb and Nd isotopes breaks down for samples with very old provenance (ɛNd<-20) that are far less radiogenic than predicted by the negative correlation. The correlations among Sr, Nd and Hf isotopes also become more scattered in samples with very old provenance. The unradiogenic Pb isotopic character of modern sediments with Archean Nd model ages is consistent with a model where Th and U abundances of the Archean upper crust are significantly lower than the post-Archean upper crust.

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

Pb isotope compositions of modern deep sea turbidites 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 Pb isotope compositions of modern deep sea turbidites, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Pb isotope compositions of modern deep sea turbidites will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-923345

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