Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean

The amount of lead annually transferred from oceanic crust to metalliferous sediments was estimated in order to test the hypothesis that a non-magmatic flux of lead causes the Pb surplus in the continental crust. A Pb surplus has been inferred from global crust-mantle lead mass balances derived from...

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Bibliographic Details
Main Authors: Peucker-Ehrenbrink, Bernhard, Hofmann, Albrecht W, Hart, Stanley R
Format: Dataset
Language:English
Published: PANGAEA 1994
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.712126
https://doi.org/10.1594/PANGAEA.712126