Partition of uranium and thorium between augite and host lavas

Details Partition of uranium and thorium between augite and host lavas Partition of uranium and thorium between augite and host lavas

Aug 1968

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968gecoa..32..917n&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 32, Issue 8, pp.917-921

Physics

3

Scientific paper

Contents of U and Th in mineral fractions separated from some volcanic lavas and a peridotite nodule have been measured. Th / U ratios were larger in the groundmass than in the augite phenocryst of the lava. In the peridotite nodule, U and Th were most enriched in diopside. Ionic substitution of Ca in clinopyroxene by U and Th under equilibrium conditions is proposed for the possible partition mechanism.

Affiliated with

Also associated with

No associations

Rating

Partition of uranium and thorium between augite and host lavas 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 Partition of uranium and thorium between augite and host lavas, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Partition of uranium and thorium between augite and host lavas will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1566004