Lead Isotope Variation with Growth Zoning in a Galena Crystal
Ralph S. Cannon Jr. 1,
Arthur P. Pierce 1, and
Maryse H. Delevaux 2
1 U. S. Geological Survey, Denver 25, Colorado
2 U. S. Geological Survey, Washington 25, D. C.
A large crystal of lead sulfide from Picher, Oklahoma, has significant differences in isotopic composition of lead in successive growth zones. Lead isotope ratios in the parent ore-fluid evidently changed with time during crystal growth. The growth history of this crystal, interpreted quantitatively, points to a tentative hypothesis of genesis of Mississippi Valley deposits of lead and zinc.